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"disqusTitle": "Geological Outings Around the Bay: Point Año Nuevo",
"title": "Geological Outings Around the Bay: Point Año Nuevo",
"headTitle": "QUEST | KQED Science",
"content": "\u003cfigure id=\"attachment_21534\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anonuevotop.jpg\" alt=\"\" title=\"anonuevotop\" width=\"640\" height=\"360\" class=\"size-full wp-image-21534\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anonuevotop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anonuevotop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003cfigcaption class=\"wp-caption-text\">Point Año Nuevo from the air, with Año Nuevo Island to its left. When Sebastian Vizcaino sighted this point on New Year's Day 1603, the island was part of the mainland.\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cem>\u003csup>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/docsearls/\">Doc Searls\u003c/a> of Flickr under Creative Commons license.\u003c/sup>\u003c/em>\u003c/p>\n\u003cp>Point Año Nuevo gets a crush of visitors during the mating season of elephant seals, a spectacle well worth the trip down the San Mateo coast. The rest of the year, especially at low tide, is good for enjoying the Point's geology. For instance, nowhere else on the California coast is a major fault zone so well exposed.\u003c/p>\n\u003cp>But first let's notice something about the Point: it's all a big flat space. In fact, looking at it from the edge, down on the beach, you'll see that it's a classic marine terrace, just like ones I've described previously at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a> a few miles to the north and at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a> in Sonoma County.\u003c/p>\n\u003cfigure id=\"attachment_21537\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anoterrace/\" rel=\"attachment wp-att-21537\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anoterrace.jpg\" alt=\"\" title=\"anoterrace\" width=\"640\" height=\"365\" class=\"size-full wp-image-21537\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoterrace.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoterrace-400x228.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The top layer of this geologic cake is a thin frosting of brown soil, some orangish stream deposits just beneath it and lighter-colored beach sands. The bottom layer is solid rock all the way down to the beach. The contact between the two layers is a strip of vegetation, where groundwater collects. That contact represents an ancient wave-cut platform, from a time about 105,000 years ago (105 ka) when the sea level was higher than today (because the glaciers had melted even more than they have today).\u003c/p>\n\u003cp>Here's a closer look at that wave-cut surface. It appears just like the modern seafloor, complete with the borings of pholad clams.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anowavecut/\" rel=\"attachment wp-att-21538\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anowavecut.jpg\" alt=\"\" title=\"anowavecut\" width=\"640\" height=\"396\" class=\"aligncenter size-full wp-image-21538\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anowavecut.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anowavecut-400x248.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The reason I could photograph this without having to climb the cliffs is that the ground in places has been faulted since 105 ka. \u003c/p>\n\u003cfigure id=\"attachment_21529\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anocutdrop/\" rel=\"attachment wp-att-21529\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anocutdrop.jpg\" alt=\"\" title=\"anocutdrop\" width=\"640\" height=\"497\" class=\"size-full wp-image-21529\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocutdrop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocutdrop-400x311.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Field trip leader Gerald Weber of UC Santa Cruz lectures at a downdropped wave-cut terrace. Behind him, this surface is several meters higher.\u003c/figcaption>\u003c/figure>\n\u003cp>Time to look at the geologic map, which shows several faults crossing Point Año Nuevo. The photo above is from the beach cliff above the word \"Bay.\"\u003c/p>\n\u003cfigure id=\"attachment_21533\" class=\"wp-caption aligncenter\" style=\"max-width: 485px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anonuevogeomap-485x360.png\" alt=\"\" title=\"anonuevogeomap\" width=\"485\" height=\"360\" class=\"size-large wp-image-21533\">\u003cfigcaption class=\"wp-caption-text\">Extracted from USGS Geologic Map of San Mateo County (http://pubs.usgs.gov/of/1998/of98-137). Click image to see a larger version. Qmt, marine terrace; Qs, dune sand; Tsc, Santa Cruz Mudstone; Tp, Purisima Formation; Qyf, active alluvial fan; gold color, older alluvial fan deposits. Año Nuevo Island is Monterey Formation.\u003c/figcaption>\u003c/figure>\n\u003cp>All of these faults are part of the San Gregorio fault zone, an obscure part of the San Andreas family that runs mostly offshore. It is thought capable of a very large magnitude 7.5 earthquake. The two most prominent strands at Point Año Nuevo are on the right-hand side of the map; they're informally named the Coastways fault (on the east) and the Frijoles fault. The Frijoles is at the center of this view:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anofrijoles/\" rel=\"attachment wp-att-21530\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anofrijoles.jpg\" alt=\"\" title=\"anofrijoles\" width=\"640\" height=\"336\" class=\"alignleft size-full wp-image-21530\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anofrijoles.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anofrijoles-400x210.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>This closeup shows where Año Nuevo Creek, long ago, took advantage of the downdrop on the fault and cut into the underlying \u003ca href=\"http://ww2.kqed.org/quest/2010/10/28/greater-bay-area-geo-attractions-san-gregorio-beach/\">Purisima Formation\u003c/a> (which is about 5 million years old). \u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anocreekcut/\" rel=\"attachment wp-att-21528\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anocreekcut.jpg\" alt=\"\" title=\"anocreekcut\" width=\"640\" height=\"373\" class=\"alignleft size-full wp-image-21528\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocreekcut.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocreekcut-400x233.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Point Año Nuevo is a very active place today, even though no large earthquakes have been documented here for about a thousand years. When first logged by European explorers in 1603, there was no island here. By the end of the 1700s there was one. Researcher Gerald Weber, who has tramped the Point since 1973, has evidence that this change created a huge washout of sand that protected the southern seacliffs of the Point until just recently. In a field trip recently, he paced off the amount he has seen the cliffs retreat since about 1980. The hat sits where renewed erosion uncovered an old pier post dating from the 1850s, when the pier served lumbering operations in the nearby hills.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anoretreat/\" rel=\"attachment wp-att-21536\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anoretreat.jpg\" alt=\"\" title=\"anoretreat\" width=\"640\" height=\"451\" class=\"alignleft size-full wp-image-21536\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoretreat.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoretreat-400x282.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Weber thinks that this sand has moved down the coast and is now affecting Santa Cruz Harbor. Eventually it will spill into Monterey Canyon and wash out to the deep sea.\u003c/p>\n\u003cp>The San Gregorio fault zone is an important mystery. This image from an old map shows its extent in this part of the San Mateo coast.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anooldgeomap/\" rel=\"attachment wp-att-21535\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anooldgeomap.jpg\" alt=\"\" title=\"anooldgeomap\" width=\"632\" height=\"273\" class=\"alignleft size-full wp-image-21535\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anooldgeomap.jpg 632w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anooldgeomap-400x173.jpg 400w\" sizes=\"(max-width: 632px) 100vw, 632px\">\u003c/a>\u003c/p>\n\u003cp>Recent mapping has improved this picture, but the work is very difficult. Lidar technology promises big advances, though. This light-based form of radar mapping allows us to strip buildings and vegetation off the underlying ground surface, making even subtle fault features stand out. Lidar imagery now covers this region:\u003c/p>\n\u003cfigure id=\"attachment_21532\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anolidarsynopt/\" rel=\"attachment wp-att-21532\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anolidarsynopt.jpg\" alt=\"\" title=\"anolidarsynopt\" width=\"640\" height=\"210\" class=\"size-full wp-image-21532\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarsynopt.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarsynopt-400x131.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Courtesy www.opentopography.org\u003c/figcaption>\u003c/figure>\n\u003cp>. . . and the Frijoles fault trace on Point Año Nuevo stands out beautifully in it.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anolidarclose/\" rel=\"attachment wp-att-21531\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anolidarclose.jpg\" alt=\"\" title=\"anolidarclose\" width=\"640\" height=\"421\" class=\"alignleft size-full wp-image-21531\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarclose.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarclose-400x263.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Learn more about Point Año Nuevo's geology from the park's \u003ca href=\"http://sanmateocoastnha.org/pages/docent_training.html\">2009 docent training materials\u003c/a>.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://opentopo.sdsc.edu/gridsphere/gridsphere?cid=otgoogleearth\">Lidar data from many Northern California fault traces\u003c/a> is freely viewable in Google Earth.\u003c/p>\n\n",
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"excerpt": "Elephant seals are seasonal attractions at Point Año Nuevo, but the geology and the earthquake hazard it presents is there year-round.",
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"headline": "Geological Outings Around the Bay: Point Año Nuevo",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_21534\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anonuevotop.jpg\" alt=\"\" title=\"anonuevotop\" width=\"640\" height=\"360\" class=\"size-full wp-image-21534\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anonuevotop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anonuevotop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003cfigcaption class=\"wp-caption-text\">Point Año Nuevo from the air, with Año Nuevo Island to its left. When Sebastian Vizcaino sighted this point on New Year's Day 1603, the island was part of the mainland.\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cem>\u003csup>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/docsearls/\">Doc Searls\u003c/a> of Flickr under Creative Commons license.\u003c/sup>\u003c/em>\u003c/p>\n\u003cp>Point Año Nuevo gets a crush of visitors during the mating season of elephant seals, a spectacle well worth the trip down the San Mateo coast. The rest of the year, especially at low tide, is good for enjoying the Point's geology. For instance, nowhere else on the California coast is a major fault zone so well exposed.\u003c/p>\n\u003cp>But first let's notice something about the Point: it's all a big flat space. In fact, looking at it from the edge, down on the beach, you'll see that it's a classic marine terrace, just like ones I've described previously at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a> a few miles to the north and at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a> in Sonoma County.\u003c/p>\n\u003cfigure id=\"attachment_21537\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anoterrace/\" rel=\"attachment wp-att-21537\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anoterrace.jpg\" alt=\"\" title=\"anoterrace\" width=\"640\" height=\"365\" class=\"size-full wp-image-21537\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoterrace.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoterrace-400x228.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The top layer of this geologic cake is a thin frosting of brown soil, some orangish stream deposits just beneath it and lighter-colored beach sands. The bottom layer is solid rock all the way down to the beach. The contact between the two layers is a strip of vegetation, where groundwater collects. That contact represents an ancient wave-cut platform, from a time about 105,000 years ago (105 ka) when the sea level was higher than today (because the glaciers had melted even more than they have today).\u003c/p>\n\u003cp>Here's a closer look at that wave-cut surface. It appears just like the modern seafloor, complete with the borings of pholad clams.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anowavecut/\" rel=\"attachment wp-att-21538\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anowavecut.jpg\" alt=\"\" title=\"anowavecut\" width=\"640\" height=\"396\" class=\"aligncenter size-full wp-image-21538\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anowavecut.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anowavecut-400x248.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The reason I could photograph this without having to climb the cliffs is that the ground in places has been faulted since 105 ka. \u003c/p>\n\u003cfigure id=\"attachment_21529\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anocutdrop/\" rel=\"attachment wp-att-21529\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anocutdrop.jpg\" alt=\"\" title=\"anocutdrop\" width=\"640\" height=\"497\" class=\"size-full wp-image-21529\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocutdrop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocutdrop-400x311.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Field trip leader Gerald Weber of UC Santa Cruz lectures at a downdropped wave-cut terrace. Behind him, this surface is several meters higher.\u003c/figcaption>\u003c/figure>\n\u003cp>Time to look at the geologic map, which shows several faults crossing Point Año Nuevo. The photo above is from the beach cliff above the word \"Bay.\"\u003c/p>\n\u003cfigure id=\"attachment_21533\" class=\"wp-caption aligncenter\" style=\"max-width: 485px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anonuevogeomap-485x360.png\" alt=\"\" title=\"anonuevogeomap\" width=\"485\" height=\"360\" class=\"size-large wp-image-21533\">\u003cfigcaption class=\"wp-caption-text\">Extracted from USGS Geologic Map of San Mateo County (http://pubs.usgs.gov/of/1998/of98-137). Click image to see a larger version. Qmt, marine terrace; Qs, dune sand; Tsc, Santa Cruz Mudstone; Tp, Purisima Formation; Qyf, active alluvial fan; gold color, older alluvial fan deposits. Año Nuevo Island is Monterey Formation.\u003c/figcaption>\u003c/figure>\n\u003cp>All of these faults are part of the San Gregorio fault zone, an obscure part of the San Andreas family that runs mostly offshore. It is thought capable of a very large magnitude 7.5 earthquake. The two most prominent strands at Point Año Nuevo are on the right-hand side of the map; they're informally named the Coastways fault (on the east) and the Frijoles fault. The Frijoles is at the center of this view:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anofrijoles/\" rel=\"attachment wp-att-21530\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anofrijoles.jpg\" alt=\"\" title=\"anofrijoles\" width=\"640\" height=\"336\" class=\"alignleft size-full wp-image-21530\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anofrijoles.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anofrijoles-400x210.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>This closeup shows where Año Nuevo Creek, long ago, took advantage of the downdrop on the fault and cut into the underlying \u003ca href=\"http://ww2.kqed.org/quest/2010/10/28/greater-bay-area-geo-attractions-san-gregorio-beach/\">Purisima Formation\u003c/a> (which is about 5 million years old). \u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anocreekcut/\" rel=\"attachment wp-att-21528\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anocreekcut.jpg\" alt=\"\" title=\"anocreekcut\" width=\"640\" height=\"373\" class=\"alignleft size-full wp-image-21528\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocreekcut.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anocreekcut-400x233.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Point Año Nuevo is a very active place today, even though no large earthquakes have been documented here for about a thousand years. When first logged by European explorers in 1603, there was no island here. By the end of the 1700s there was one. Researcher Gerald Weber, who has tramped the Point since 1973, has evidence that this change created a huge washout of sand that protected the southern seacliffs of the Point until just recently. In a field trip recently, he paced off the amount he has seen the cliffs retreat since about 1980. The hat sits where renewed erosion uncovered an old pier post dating from the 1850s, when the pier served lumbering operations in the nearby hills.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anoretreat/\" rel=\"attachment wp-att-21536\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anoretreat.jpg\" alt=\"\" title=\"anoretreat\" width=\"640\" height=\"451\" class=\"alignleft size-full wp-image-21536\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoretreat.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anoretreat-400x282.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Weber thinks that this sand has moved down the coast and is now affecting Santa Cruz Harbor. Eventually it will spill into Monterey Canyon and wash out to the deep sea.\u003c/p>\n\u003cp>The San Gregorio fault zone is an important mystery. This image from an old map shows its extent in this part of the San Mateo coast.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anooldgeomap/\" rel=\"attachment wp-att-21535\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anooldgeomap.jpg\" alt=\"\" title=\"anooldgeomap\" width=\"632\" height=\"273\" class=\"alignleft size-full wp-image-21535\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anooldgeomap.jpg 632w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anooldgeomap-400x173.jpg 400w\" sizes=\"(max-width: 632px) 100vw, 632px\">\u003c/a>\u003c/p>\n\u003cp>Recent mapping has improved this picture, but the work is very difficult. Lidar technology promises big advances, though. This light-based form of radar mapping allows us to strip buildings and vegetation off the underlying ground surface, making even subtle fault features stand out. Lidar imagery now covers this region:\u003c/p>\n\u003cfigure id=\"attachment_21532\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anolidarsynopt/\" rel=\"attachment wp-att-21532\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anolidarsynopt.jpg\" alt=\"\" title=\"anolidarsynopt\" width=\"640\" height=\"210\" class=\"size-full wp-image-21532\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarsynopt.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarsynopt-400x131.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Courtesy www.opentopography.org\u003c/figcaption>\u003c/figure>\n\u003cp>. . . and the Frijoles fault trace on Point Año Nuevo stands out beautifully in it.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/07/28/geological-outings-around-the-bay-point-ao-nuevo/anolidarclose/\" rel=\"attachment wp-att-21531\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/anolidarclose.jpg\" alt=\"\" title=\"anolidarclose\" width=\"640\" height=\"421\" class=\"alignleft size-full wp-image-21531\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarclose.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/anolidarclose-400x263.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Learn more about Point Año Nuevo's geology from the park's \u003ca href=\"http://sanmateocoastnha.org/pages/docent_training.html\">2009 docent training materials\u003c/a>.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://opentopo.sdsc.edu/gridsphere/gridsphere?cid=otgoogleearth\">Lidar data from many Northern California fault traces\u003c/a> is freely viewable in Google Earth.\u003c/p>\n\n\u003c/div>\u003c/p>",
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"content": "\u003cfigure id=\"attachment_20958\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca rel=\"attachment wp-att-20958\" href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/cinnabar/\">\u003cimg class=\"size-thumbnail wp-image-20958\" title=\"cinnabar\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/cinnabar-300x169.jpg\" alt=\"\" width=\"300\" height=\"169\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Cinnabar from Lake County. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>It's widely known that California has a mercury problem unlike other parts of the world. We don't produce it and we don't emit much any more, but a lot of old mercury is still lying around from the mining days. How did that happen?\u003c/p>\n\u003cp>In undisturbed nature, mercury is no more than a very local and very temporary problem. Mercury occurs mostly in sulfide compounds that are concentrated where ore-forming fluids invade metal-rich rocks. Cinnabar and metacinnabar are both mercury sulfide, HgS. Metacinnabar forms at higher temperatures.\u003c/p>\n\u003cfigure id=\"attachment_20957\" class=\"wp-caption alignnone\" style=\"max-width: 640px\">\u003ca rel=\"attachment wp-att-20957\" href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/metacinnabar/\">\u003cimg class=\"size-full wp-image-20957\" title=\"metacinnabar\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/metacinnabar.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/metacinnabar.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/metacinnabar-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Metacinnabar from the Mt. Diablo Mine. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>The California Coast Range was a natural place for world-class mercury ore bodies to grow. First, the range has a large amount of metal-rich rocks in the form of serpentinite and its parent rock, peridotite, derived from ancient seafloor. Second, these rocks were cracked and tilted as the Coast Range was built. Third, volcanic activity worked over these rocks, adding heat and chemically active fluids. Thus the source rocks were repeatedly mobilized, attacked and disrupted, a natural refining sequence that at each step concentrated metals.\u003c/p>\n\u003cp>Serpentinite is a slippery rock that tends to attract faults, which in turn attract fluids. Hot deep fluids replaced the serpentinite with carbonate minerals like calcite, then again with silicate minerals like quartz. As veins of these minerals fan outward they carry mercury with them. Coast Range mercury was originally deposited at high temperatures deep underground, often associated with gold sitting a bit deeper. It remains for erosion to slowly uncover the ores. In coastal California, erosion is quite active as the Coast Range continues to rise.\u003c/p>\n\u003cp>Wide zones of silica-carbonate alteration dot our mountains and host hundreds of mercury occurrences. The great New Almaden Mine, south of San Jose, exploited a deposit of this type. It was the largest mercury producer in North America, spawning the gold mining industry that followed the placer gold rush of 1849. Cheap, efficient mercury amalgamation was the key to gold production, and New Almaden mercury made it feasible.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Volcanic heat also spawns hot-spring activity that can create mercury ore bodies, too. The \u003ca href=\"http://nrs.ucdavis.edu/mcl/natural/geology/geo.htm\">McLaughlin Mine\u003c/a>, north of Lake Berryessa, exploited a hot-spring type deposit yielding gold as well as mercury.\u003c/p>\n\u003cp>Today the mercury mines of the Bay Area are all closed and being remediated. The \u003ca href=\"http://www.newalmaden.org/\">New Almaden property\u003c/a> is now a county park and the McLaughlin Mine is being carefully restored to a working countryside. Fortunately, mercury can be well controlled if acid mine drainage can be prevented, because cinnabar is poorly soluble except in strongly acid waters. At Clear Lake, the large former \u003ca href=\"http://en.wikipedia.org/wiki/Sulphur_Bank_Mine\">Sulphur Bank Mine\u003c/a> is slowly getting under control. The privately owned \u003ca href=\"http://www.google.com/url?sa=t&source=web&cd=7&ved=0CEYQFjAG&url=http%3A%2F%2Fwww.prpblog.com%2Fmtdiablo%2Fdownloads%2FMount%2520Diablo%2527s%2520mercury%2520mine...pdf&ei=ZW8oToKjFIvWtQP7wtDzCA&usg=AFQjCNHfcsM_OHK6kHauUROLyWpA4vVmRg&sig2=KMxH-RJgFPbVUP5sk2ZWBQ\">Mount Diablo Mine\u003c/a>, where my metacinnabar specimen was collected, is not a threat to spill into local streams although money is needed to fix it for good.\u003c/p>\n\u003cp>Worldwide, the overwhelmingly largest source of mercury pollution is from the burning of coal. A much smaller source is from oil and gas. Mercury appears to ride along with oil and gas as they trickle from their source rocks upward into the reservoirs we mine for energy. In oil, mercury lives in the tiny metal portion; in gas, mercury is a vapor. Levels in both are in the low parts-per-billion range, although California's oil tends to have relatively high levels. Mercury levels are highest in the dense fraction called petroleum coke, which is burned in place of coal. Even so, coal is far dirtier in terms of mercury, and the Bay Area is spared that insult.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003cstrong>More reading:\u003c/strong>\u003c/p>\n\u003cul>\n\u003cli>\u003ca href=\"http://www.esajournals.org/toc/ecap/18/sp8\">Mercury Cycling and Bioaccumulation in Clear Lake\u003c/a>, special issue of \u003cem>Ecological Applications\u003c/em>\u003c/li>\n\u003cli>\u003ca href=\"http://pubs.usgs.gov/of/2002/of02-195/OF02-195J.pdf\">Mercury Geoenvironmental Models\u003c/a> by James Rytuba (US Geological Survey)\u003c/li>\n\u003c/ul>\n\n",
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"excerpt": "The Bay Area's mercury problem arises from the special geology of the Coast Range that concentrates the metal in the mineral cinnabar.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_20958\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca rel=\"attachment wp-att-20958\" href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/cinnabar/\">\u003cimg class=\"size-thumbnail wp-image-20958\" title=\"cinnabar\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/cinnabar-300x169.jpg\" alt=\"\" width=\"300\" height=\"169\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Cinnabar from Lake County. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>It's widely known that California has a mercury problem unlike other parts of the world. We don't produce it and we don't emit much any more, but a lot of old mercury is still lying around from the mining days. How did that happen?\u003c/p>\n\u003cp>In undisturbed nature, mercury is no more than a very local and very temporary problem. Mercury occurs mostly in sulfide compounds that are concentrated where ore-forming fluids invade metal-rich rocks. Cinnabar and metacinnabar are both mercury sulfide, HgS. Metacinnabar forms at higher temperatures.\u003c/p>\n\u003cfigure id=\"attachment_20957\" class=\"wp-caption alignnone\" style=\"max-width: 640px\">\u003ca rel=\"attachment wp-att-20957\" href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/metacinnabar/\">\u003cimg class=\"size-full wp-image-20957\" title=\"metacinnabar\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/metacinnabar.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/metacinnabar.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/metacinnabar-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Metacinnabar from the Mt. Diablo Mine. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>The California Coast Range was a natural place for world-class mercury ore bodies to grow. First, the range has a large amount of metal-rich rocks in the form of serpentinite and its parent rock, peridotite, derived from ancient seafloor. Second, these rocks were cracked and tilted as the Coast Range was built. Third, volcanic activity worked over these rocks, adding heat and chemically active fluids. Thus the source rocks were repeatedly mobilized, attacked and disrupted, a natural refining sequence that at each step concentrated metals.\u003c/p>\n\u003cp>Serpentinite is a slippery rock that tends to attract faults, which in turn attract fluids. Hot deep fluids replaced the serpentinite with carbonate minerals like calcite, then again with silicate minerals like quartz. As veins of these minerals fan outward they carry mercury with them. Coast Range mercury was originally deposited at high temperatures deep underground, often associated with gold sitting a bit deeper. It remains for erosion to slowly uncover the ores. In coastal California, erosion is quite active as the Coast Range continues to rise.\u003c/p>\n\u003cp>Wide zones of silica-carbonate alteration dot our mountains and host hundreds of mercury occurrences. The great New Almaden Mine, south of San Jose, exploited a deposit of this type. It was the largest mercury producer in North America, spawning the gold mining industry that followed the placer gold rush of 1849. Cheap, efficient mercury amalgamation was the key to gold production, and New Almaden mercury made it feasible.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Volcanic heat also spawns hot-spring activity that can create mercury ore bodies, too. The \u003ca href=\"http://nrs.ucdavis.edu/mcl/natural/geology/geo.htm\">McLaughlin Mine\u003c/a>, north of Lake Berryessa, exploited a hot-spring type deposit yielding gold as well as mercury.\u003c/p>\n\u003cp>Today the mercury mines of the Bay Area are all closed and being remediated. The \u003ca href=\"http://www.newalmaden.org/\">New Almaden property\u003c/a> is now a county park and the McLaughlin Mine is being carefully restored to a working countryside. Fortunately, mercury can be well controlled if acid mine drainage can be prevented, because cinnabar is poorly soluble except in strongly acid waters. At Clear Lake, the large former \u003ca href=\"http://en.wikipedia.org/wiki/Sulphur_Bank_Mine\">Sulphur Bank Mine\u003c/a> is slowly getting under control. The privately owned \u003ca href=\"http://www.google.com/url?sa=t&source=web&cd=7&ved=0CEYQFjAG&url=http%3A%2F%2Fwww.prpblog.com%2Fmtdiablo%2Fdownloads%2FMount%2520Diablo%2527s%2520mercury%2520mine...pdf&ei=ZW8oToKjFIvWtQP7wtDzCA&usg=AFQjCNHfcsM_OHK6kHauUROLyWpA4vVmRg&sig2=KMxH-RJgFPbVUP5sk2ZWBQ\">Mount Diablo Mine\u003c/a>, where my metacinnabar specimen was collected, is not a threat to spill into local streams although money is needed to fix it for good.\u003c/p>\n\u003cp>Worldwide, the overwhelmingly largest source of mercury pollution is from the burning of coal. A much smaller source is from oil and gas. Mercury appears to ride along with oil and gas as they trickle from their source rocks upward into the reservoirs we mine for energy. In oil, mercury lives in the tiny metal portion; in gas, mercury is a vapor. Levels in both are in the low parts-per-billion range, although California's oil tends to have relatively high levels. Mercury levels are highest in the dense fraction called petroleum coke, which is burned in place of coal. Even so, coal is far dirtier in terms of mercury, and the Bay Area is spared that insult.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003cstrong>More reading:\u003c/strong>\u003c/p>\n\u003cul>\n\u003cli>\u003ca href=\"http://www.esajournals.org/toc/ecap/18/sp8\">Mercury Cycling and Bioaccumulation in Clear Lake\u003c/a>, special issue of \u003cem>Ecological Applications\u003c/em>\u003c/li>\n\u003cli>\u003ca href=\"http://pubs.usgs.gov/of/2002/of02-195/OF02-195J.pdf\">Mercury Geoenvironmental Models\u003c/a> by James Rytuba (US Geological Survey)\u003c/li>\n\u003c/ul>\n\n\u003c/div>\u003c/p>",
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"disqusTitle": "Petroleum in the Bay Area",
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"content": "\u003cfigure id=\"attachment_20136\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepbakersfield.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepbakersfield-300x169.jpg\" alt=\"\" title=\"seepbakersfield\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-20136\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Oil wells creak in the Bakersfield twilight. Petroleum is not confined to Southern California and Central Valley; we have it in the Bay Area too. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>Norma Desmond, the washed-up movie star of \u003ci>Sunset Boulevard\u003c/i>, had some memorable lines. One of them was, \"I've got oil wells in Bakersfield, pumping pumping pumping.\" We think of our petroleum as a Southern California thing, or at least no closer than the Great Valley. But petroleumoil and gas, or bothis widespread around the state, including the Bay Area.\u003c/p>\n\u003cp>It wasn't just gold, water and agricultural soils that made California rich. Petroleum is one of our greatest natural assets, and the state still ranks fourth in oil production behind Louisiana, Texas and Alaska. While the forests of derricks that once dotted Los Angeles are now subdued and disguised, the Central Valley is still a proud petroleum region, with gas fields in the Sacramento Valley and oil fields in the San Joaquin Valley.\u003c/p>\n\u003cp>The oil and gas fields of the Central Valley intrude into the Bay Area from the Delta as far as Concord and the Suisun Bay to its north. Gas was produced from the hills north of Concord in the 1960s, and today the old Los Medanos gas field is used by PG&E for storage.\u003c/p>\n\u003cfigure id=\"attachment_20138\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepdrip/\" rel=\"attachment wp-att-20138\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepdrip.jpg\" alt=\"\" title=\"seepdrip\" width=\"500\" height=\"342\" class=\"size-full wp-image-20138\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepdrip.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepdrip-400x274.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo (c) 2007 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Before petroleum exploration became high-tech, the best way to find oil and gas was to look for natural seeps. An oily sheen on a stream, trickles of tar from a sunny sea cliff, and persistent odors like kerosene are typical signs. These are more common than most people think. Much rarer are actual tar flows like those at Carpinteria Beach near Santa Barbara.\u003c/p>\n\u003cfigure id=\"attachment_20137\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepcarptar/\" rel=\"attachment wp-att-20137\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepcarptar.jpg\" alt=\"\" title=\"seepcarptar\" width=\"500\" height=\"321\" class=\"size-full wp-image-20137\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepcarptar.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepcarptar-400x257.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo (c) 2010 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Oil seeps were discovered near Half Moon Bay and in the Santa Cruz Mountains in the 1800s. Asphalt and tar sand were mined from these areas for the streets of San Francisco. \u003c/p>\n\u003cfigure id=\"attachment_20135\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepasphalt/\" rel=\"attachment wp-att-20135\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepasphalt.jpg\" alt=\"\" title=\"seepasphalt\" width=\"500\" height=\"322\" class=\"size-full wp-image-20135\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepasphalt.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepasphalt-400x258.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Natural asphalt from the McKittrick tar seep. Photo by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Later, conventional exploration opened up four districts of producing wells in the San Mateo Peninsula: the Half Moon Bay, La Honda and Oil Creek fields still yield oil today. The Moody Gulch field, which started as a tar pit in 1878, was shut down in 1960 and is now under Route 17.\u003c/p>\n\u003cfigure id=\"attachment_20140\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepstop/\" rel=\"attachment wp-att-20140\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepstop.jpg\" alt=\"\" hspace=\"5\" title=\"seepstop\" width=\"300\" height=\"200\" class=\"alignleft size-full wp-image-20140\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo by Les Magoon, U.S. Geological Survey\u003c/figcaption>\u003c/figure>\n\u003cp>The North Bay has petroleum too. This natural gas seep in Mendocino County is used by the locals as a built-in campfire (photo by Les Magoon, US Geological Survey). Gas and oil seeps were found early on Point Reyes, where one gas seep between Double Point and Duxbury Point was reported as \"big enough to cook fish on when lighted.\" The same rocks, also bearing dikes of oil-soaked sandstone, appear near Davenport on the San Mateo County coast, attesting to movement on the San Andreas fault system.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Elsewhere in the Bay Area, oil and gas have been produced in Petaluma, Pinole and Livermore. Oil was reported in the \u003ca href=\"http://ww2.kqed.org/quest/2011/05/26/new-fossils-from-the-caldecott-tunnel/\">Caldecott Tunnel excavations\u003c/a>, which is to be expected as the tunnel penetrates our local piece of the Monterey Formation, a petroleum source rock of great extent.\u003c/p>\n\u003cp>Oil and gas are called fossil fuels, but maybe a better concept is that they are geological compost. They are the bodies of dead plankton, trapped in the mud with no oxygen to consume them. Instead their living substance breaks down and is transformed into simpler hydrocarbon compounds. \u003c/p>\n\u003cp>The simplest and lightest of these is methane, and that's refined and sold to us as \"natural gas.\" But actual natural gas, the stuff bubbling up in tar pits, is a mixture of compounds. It won't smell like the gas in your stovethat smell is the odorant butyl mercaptan. It's more like the smell of crude oila tantalizing, sweeter version of your local gas station. If you don't know how crude oil smells, take a side trip to the oil fields on your way south, like this one just off Interstate 5 at Lost Hills.\u003c/p>\n\u003cfigure id=\"attachment_20139\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seeplosthills/\" rel=\"attachment wp-att-20139\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seeplosthills.jpg\" alt=\"\" title=\"seeplosthills\" width=\"500\" height=\"242\" class=\"size-full wp-image-20139\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seeplosthills.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seeplosthills-400x194.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Lost Hills oil field. Photo (c) 2010 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>The U.S. Geological Survey has a wealth of material on California's oil and gas seeps at \u003ca href=\"http://walrus.wr.usgs.gov/seeps/\">walrus.wr.usgs.gov/seeps\u003c/a>.\u003c/p>\n\n",
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"excerpt": "California's early oil districts included Half Moon Bay and the Santa Cruz Mountains. You can still find oil and gas around these parts.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_20136\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepbakersfield.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepbakersfield-300x169.jpg\" alt=\"\" title=\"seepbakersfield\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-20136\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Oil wells creak in the Bakersfield twilight. Petroleum is not confined to Southern California and Central Valley; we have it in the Bay Area too. Photo by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>Norma Desmond, the washed-up movie star of \u003ci>Sunset Boulevard\u003c/i>, had some memorable lines. One of them was, \"I've got oil wells in Bakersfield, pumping pumping pumping.\" We think of our petroleum as a Southern California thing, or at least no closer than the Great Valley. But petroleumoil and gas, or bothis widespread around the state, including the Bay Area.\u003c/p>\n\u003cp>It wasn't just gold, water and agricultural soils that made California rich. Petroleum is one of our greatest natural assets, and the state still ranks fourth in oil production behind Louisiana, Texas and Alaska. While the forests of derricks that once dotted Los Angeles are now subdued and disguised, the Central Valley is still a proud petroleum region, with gas fields in the Sacramento Valley and oil fields in the San Joaquin Valley.\u003c/p>\n\u003cp>The oil and gas fields of the Central Valley intrude into the Bay Area from the Delta as far as Concord and the Suisun Bay to its north. Gas was produced from the hills north of Concord in the 1960s, and today the old Los Medanos gas field is used by PG&E for storage.\u003c/p>\n\u003cfigure id=\"attachment_20138\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepdrip/\" rel=\"attachment wp-att-20138\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepdrip.jpg\" alt=\"\" title=\"seepdrip\" width=\"500\" height=\"342\" class=\"size-full wp-image-20138\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepdrip.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepdrip-400x274.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo (c) 2007 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Before petroleum exploration became high-tech, the best way to find oil and gas was to look for natural seeps. An oily sheen on a stream, trickles of tar from a sunny sea cliff, and persistent odors like kerosene are typical signs. These are more common than most people think. Much rarer are actual tar flows like those at Carpinteria Beach near Santa Barbara.\u003c/p>\n\u003cfigure id=\"attachment_20137\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepcarptar/\" rel=\"attachment wp-att-20137\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepcarptar.jpg\" alt=\"\" title=\"seepcarptar\" width=\"500\" height=\"321\" class=\"size-full wp-image-20137\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepcarptar.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepcarptar-400x257.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo (c) 2010 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Oil seeps were discovered near Half Moon Bay and in the Santa Cruz Mountains in the 1800s. Asphalt and tar sand were mined from these areas for the streets of San Francisco. \u003c/p>\n\u003cfigure id=\"attachment_20135\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepasphalt/\" rel=\"attachment wp-att-20135\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepasphalt.jpg\" alt=\"\" title=\"seepasphalt\" width=\"500\" height=\"322\" class=\"size-full wp-image-20135\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepasphalt.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seepasphalt-400x258.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Natural asphalt from the McKittrick tar seep. Photo by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Later, conventional exploration opened up four districts of producing wells in the San Mateo Peninsula: the Half Moon Bay, La Honda and Oil Creek fields still yield oil today. The Moody Gulch field, which started as a tar pit in 1878, was shut down in 1960 and is now under Route 17.\u003c/p>\n\u003cfigure id=\"attachment_20140\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seepstop/\" rel=\"attachment wp-att-20140\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seepstop.jpg\" alt=\"\" hspace=\"5\" title=\"seepstop\" width=\"300\" height=\"200\" class=\"alignleft size-full wp-image-20140\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photo by Les Magoon, U.S. Geological Survey\u003c/figcaption>\u003c/figure>\n\u003cp>The North Bay has petroleum too. This natural gas seep in Mendocino County is used by the locals as a built-in campfire (photo by Les Magoon, US Geological Survey). Gas and oil seeps were found early on Point Reyes, where one gas seep between Double Point and Duxbury Point was reported as \"big enough to cook fish on when lighted.\" The same rocks, also bearing dikes of oil-soaked sandstone, appear near Davenport on the San Mateo County coast, attesting to movement on the San Andreas fault system.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Elsewhere in the Bay Area, oil and gas have been produced in Petaluma, Pinole and Livermore. Oil was reported in the \u003ca href=\"http://ww2.kqed.org/quest/2011/05/26/new-fossils-from-the-caldecott-tunnel/\">Caldecott Tunnel excavations\u003c/a>, which is to be expected as the tunnel penetrates our local piece of the Monterey Formation, a petroleum source rock of great extent.\u003c/p>\n\u003cp>Oil and gas are called fossil fuels, but maybe a better concept is that they are geological compost. They are the bodies of dead plankton, trapped in the mud with no oxygen to consume them. Instead their living substance breaks down and is transformed into simpler hydrocarbon compounds. \u003c/p>\n\u003cp>The simplest and lightest of these is methane, and that's refined and sold to us as \"natural gas.\" But actual natural gas, the stuff bubbling up in tar pits, is a mixture of compounds. It won't smell like the gas in your stovethat smell is the odorant butyl mercaptan. It's more like the smell of crude oila tantalizing, sweeter version of your local gas station. If you don't know how crude oil smells, take a side trip to the oil fields on your way south, like this one just off Interstate 5 at Lost Hills.\u003c/p>\n\u003cfigure id=\"attachment_20139\" class=\"wp-caption alignnone\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/07/14/petroleum-in-the-bay-area/seeplosthills/\" rel=\"attachment wp-att-20139\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/seeplosthills.jpg\" alt=\"\" title=\"seeplosthills\" width=\"500\" height=\"242\" class=\"size-full wp-image-20139\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/07/seeplosthills.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/07/seeplosthills-400x194.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Lost Hills oil field. Photo (c) 2010 Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>The U.S. Geological Survey has a wealth of material on California's oil and gas seeps at \u003ca href=\"http://walrus.wr.usgs.gov/seeps/\">walrus.wr.usgs.gov/seeps\u003c/a>.\u003c/p>\n\n\u003c/div>\u003c/p>",
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"disqusTitle": "Geological Outings Around the Bay: The Great Slickenside of Corona Heights",
"title": "Geological Outings Around the Bay: The Great Slickenside of Corona Heights",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronatop.jpg\" alt=\"corona heights\" class=\"alignleft size-full\">\u003cem>\u003csup>Sutro Tower and the gnarled chert of the Marin Headlandsterrane are parts of a splendid spectacle at San Francisco's Corona Heights. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>San Francisco is \"America's Favorite City\" for many great reasons. Geologists have their own list of reasons to love it, many of which are Franciscan—by which we mean the peculiar association of rocks found up and down the Coast Ranges. Corona Heights is a small hill west of the Castro district that features some of these rocks, but one of its main attractions is a world-class slickenside.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>You get to Corona Heights by walking about a mile west from the 16th/Mission BART station, or by taking the F line up Market Street to the Noe or Sanchez stops. Here's the hill as seen from 16th Street. You can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona1.jpg\" alt=\"corona heights\">\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Corona Heights is a hardworking hill that formerly yielded clay and chert. Years of quarrying have accentuated its rugged appearance and left splendid exposures of the bedrock. Along the way, if you keep an eye on appearances of old concrete (doesn't everybody?), you may spot the old chert aggregate around the neighborhood.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona2.jpg\" alt=\"chert aggregate\">\u003c/p>\n\u003cp>Corona Heights, like Bernal Heights to the southeast, is an island of resistant chert that is part of the dismembered \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands terrane\u003c/a>. It houses a fine playground and the \u003ca href=\"http://www.randallmuseum.org/\">Randall Museum\u003c/a>. It has a \u003ca href=\"http://sfnaturalareas.org/pages/1\">dedicated group doing habitat restoration\u003c/a>. But we're here to see the slickenside.\u003c/p>\n\u003cp>A slickenside is the polished surface that is created along a fault as the rocks rub against each other. They are common in faulted rocks, but only in patches the size of your hand. (I showed you some in \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">the Calera Limestone\u003c/a>.) Larger ones are rarer. Quarrying at Corona Heights uncovered one the size of a big front yard, one of the world's largest exposures. To see it, start at Castro and 15th, go uphill on 15th and turn left on Beaver Street. Again, you can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona3.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>The site is also a playground, named for Sidney Peixotto. If you continue up 15th Street instead, you'll see the exposure this way.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona4.jpg\" alt=\"playground and slickenside\">\u003c/p>\n\u003cp>But the real joy of the thing comes at close hand, where you can feel the mirror-smooth surface that only a hard stone like chert can provide.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona5.jpg\" alt=\"fault polish\">\u003c/p>\n\u003cp>Surfaces like this are of scientific interest, although the data base is still scant. UC Santa Cruz researcher James Kirkpatrick has surveyed this site by lidar. He and others hope that close analysis can tell us more about how faults behave in detail. That's an advanced topic; the rest of us can \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?guid=52f407dc-3635-46b9-89e5-1564c28b4578\">collect the geocache at this spot\u003c/a>.\u003c/p>\n\u003cp>Afterward is a good time to climb to the top of the hill and take in one of the city's best views. On a clear day you can see \u003ca href=\"http://www.kqed.org/quest/blog/2011/06/02/mount-diablo-views/\">Mount Diablo\u003c/a> (click for a 1000-pixel version).\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\" width=\"500\" alt=\"panorama\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.7654 -122.4373\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronatop.jpg\" alt=\"corona heights\" class=\"alignleft size-full\">\u003cem>\u003csup>Sutro Tower and the gnarled chert of the Marin Headlandsterrane are parts of a splendid spectacle at San Francisco's Corona Heights. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>San Francisco is \"America's Favorite City\" for many great reasons. Geologists have their own list of reasons to love it, many of which are Franciscan—by which we mean the peculiar association of rocks found up and down the Coast Ranges. Corona Heights is a small hill west of the Castro district that features some of these rocks, but one of its main attractions is a world-class slickenside.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>You get to Corona Heights by walking about a mile west from the 16th/Mission BART station, or by taking the F line up Market Street to the Noe or Sanchez stops. Here's the hill as seen from 16th Street. You can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona1.jpg\" alt=\"corona heights\">\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Corona Heights is a hardworking hill that formerly yielded clay and chert. Years of quarrying have accentuated its rugged appearance and left splendid exposures of the bedrock. Along the way, if you keep an eye on appearances of old concrete (doesn't everybody?), you may spot the old chert aggregate around the neighborhood.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona2.jpg\" alt=\"chert aggregate\">\u003c/p>\n\u003cp>Corona Heights, like Bernal Heights to the southeast, is an island of resistant chert that is part of the dismembered \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands terrane\u003c/a>. It houses a fine playground and the \u003ca href=\"http://www.randallmuseum.org/\">Randall Museum\u003c/a>. It has a \u003ca href=\"http://sfnaturalareas.org/pages/1\">dedicated group doing habitat restoration\u003c/a>. But we're here to see the slickenside.\u003c/p>\n\u003cp>A slickenside is the polished surface that is created along a fault as the rocks rub against each other. They are common in faulted rocks, but only in patches the size of your hand. (I showed you some in \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">the Calera Limestone\u003c/a>.) Larger ones are rarer. Quarrying at Corona Heights uncovered one the size of a big front yard, one of the world's largest exposures. To see it, start at Castro and 15th, go uphill on 15th and turn left on Beaver Street. Again, you can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona3.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>The site is also a playground, named for Sidney Peixotto. If you continue up 15th Street instead, you'll see the exposure this way.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona4.jpg\" alt=\"playground and slickenside\">\u003c/p>\n\u003cp>But the real joy of the thing comes at close hand, where you can feel the mirror-smooth surface that only a hard stone like chert can provide.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona5.jpg\" alt=\"fault polish\">\u003c/p>\n\u003cp>Surfaces like this are of scientific interest, although the data base is still scant. UC Santa Cruz researcher James Kirkpatrick has surveyed this site by lidar. He and others hope that close analysis can tell us more about how faults behave in detail. That's an advanced topic; the rest of us can \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?guid=52f407dc-3635-46b9-89e5-1564c28b4578\">collect the geocache at this spot\u003c/a>.\u003c/p>\n\u003cp>Afterward is a good time to climb to the top of the hill and take in one of the city's best views. On a clear day you can see \u003ca href=\"http://www.kqed.org/quest/blog/2011/06/02/mount-diablo-views/\">Mount Diablo\u003c/a> (click for a 1000-pixel version).\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\" width=\"500\" alt=\"panorama\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.7654 -122.4373\u003c/p>\n\n\u003c/div>\u003c/p>",
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"disqusTitle": "Is the Salton Sea really "15 Months Pregnant" with our next big quake?",
"title": "Is the Salton Sea really "15 Months Pregnant" with our next big quake?",
"headTitle": "QUEST | KQED Science",
"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltontop1.jpg\" alt=\"lake cahuilla\" class=\"alignleft size-full\">\u003cem>\u003csup>The carbonate crust called tufa coats a high boulder over the Salton Sea, testifying that the Colorado River fed mighty Lake Cahuilla there in the geologically recent past. Photo by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Geologic research is a remote and dusty undertaking that can look tedious to most people. But if it bears on subjects we fear, like earthquakes, even painstaking background projects can be blown out of proportion. A recent example from Southern California went from an intriguing journal article to \"we're all gonna die\" TV stories in the space of a day. Maybe it will help you spot the next time this happens in the Bay Area.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The article, published in the prestigious \u003ci>Nature Geoscience\u003c/i> on June 26, presented the fruits of years of heat and tedium on the foul waters of the Salton Sea, in southernmost California. The Salton Sea occupies a sinking basin, the Salton Trough, that would rather be part of the Sea of Cortez except that the Colorado River has built a delta that dams it dry. As the river wanders over its delta, draining sometimes south and sometimes north, it periodically creates a geologically temporary lake in the Salton basin that has filled and dried out many times in the last few million years. (\u003ca href=\"http://www.youtube.com/watch?v=4RHu2h5CF9s\">A short video\u003c/a> by the University of Redlands illustrates the process.) \u003c/p>\n\u003cp>The repeating lake is known as Lake Cahuilla, and the Salton Sea is today's version of it. The Salton Sea is actually a terrible blunder, formed in 1905 when an irrigation canal tapping the Colorado River burst its banks and flooded a huge area of farmland in the dry bed of Lake Cahuilla. The breach was eventually fixed before the reborn lake could drown everything from Mexicali to Indio, but floods continued to be a problem until Hoover Dam was built upstream 30 years later.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The Salton Sea covers up the southern end of the San Andreas fault, and that's where our science story begins. A research team from Scripps Institution of Oceanography crisscrossed the drowned land in a small boat with a state-of-the-art CHIRP sonar system. They mapped a swarm of short faults running from the end of the San Andreas toward the end of the Imperial fault lying to the south—a tectonic configuration called a stepover. Here's the figure showing how it all fits together.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltonmap1.gif\" alt=\"salton sea tectonics\">\u003cbr>\n\u003csub>Tectonic setting of the Salton Trough and Salton Sea. SJF is San Jacinto fault, SSAF is southern San Andreas fault and IF is Imperial fault. Green grid is ship tracks in the dashed box; awz (acoustic wipeout zone) marks disturbed sediments. (Scripps)\u003c/sub>\u003c/p>\n\u003cp>From their sonar database the researchers extracted a decent record of recent ruptures on some of these stepover faults. My figure below shows, schematically, how the sediment record is built as downdrops on the fault combine with sediment being deposited on top. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltonprofiles1.gif\" alt=\"fault offset sediment record\">\u003c/p>\n\u003cp>The researchers ran this process backward to reconstruct the history of faulting for a few thousand years into the past.\u003c/p>\n\u003cp>What made things interesting was how this record of stepover quakes meshed with records of lake floods and San Andreas mega-quakes. The correlation is imperfect, but intriguing: every time the lake was reborn in a flood, the stepover faults gave way, and half of the recent mega-quakes coincided with stepover quakes. To connect the dots further, the researchers said that \"at least one of the last three dry-basin floods coincides with an earthquake on the SSAF (southern San Andreas fault).\" In their cautious words, \"We propose that loading by (Lake Cahuilla) may have induced failure on faults beneath the Salton Sea that, in turn, has the potential to trigger an earthquake rupture on the SSAF.\"\u003c/p>\n\u003cp>That's all ingenious science (seismic oceanography, in the desert!), but not news. To get news takes a press officer with a nose for a hook, and the hook is that the SSAF hasn't broken in some 300 years when we might (given the recent record) expect it to happen more often. Has our failure to let Lake Cahuilla be reborn held off triggering the next Big One? Well, has it?? \u003c/p>\n\u003cp>That question is something for geologists to wave their arms about at meetings and parties, not hold out to the world as a sure thing. But between the paper, \u003ca href=\"http://www.nature.com/ngeo/journal/vaop/ncurrent/full/ngeo1184.html\">whose abstract is world-readable\u003c/a>, and the \u003ca href=\"http://www.eurekalert.org/pub_releases/2011-06/uoc--foa062411.php\">press release from Scripps\u003c/a> we can see the story begin to morph. It's a scattershot press release, meant to serve any news angle, that immediately confuses today's managed Salton Sea with wild prehistoric Lake Cahuilla. It includes a great hook, a quote about the \"overdue\" SSAF likening it to \"a woman who is 15 months pregnant.\" The quote is only part of the background to the science, just a tangential part of the paper itself, but irresistible to the troutlike mind of the news reporter.\u003c/p>\n\u003cp>First out the chute on June 26 was \u003ca href=\"http://www.signonsandiego.com/news/2011/jun/26/salton-sea-poses-big-earthquake-threat-southern-ca/\">the \u003cem>San Diego Union-Tribune\u003c/em>'s website\u003c/a>, where Gary Robbins immediately removed all scientific uncertainty in his first sentence: \"The Salton Sea east of San Diego is a deceptively dangerous backwater, hiding faults that repeatedly produce powerful earthquakes that jolt all of Southern California, says a new study by the Scripps Institution of Oceanography.\" \u003c/p>\n\u003cp>Later that day a Los Angeles TV station rewrote Robbins's story under the headline \"\u003ca href=\"http://www.nbclosangeles.com/news/local/River-Diversions-could-lead-to-Megaquake-124595454.html\">Mega Quake Around the Corner?\u003c/a>\" with the lead sentence, \"Man's interference with Colorado River floods that used to regularly flow to the Salton Sea may have 'stopped the clock' on a regular series of big earthquakes, setting the stage for a mega quake that could wreck Southern California, scientists said Sunday.\" The accidental flood of 1905 has become \"interference\" with regular flows to the Salton Sea, and the reasoning has turned upside-down: If we had let the Imperial Valley drown, Southern California's \"Big One\" might already have happened and been a few tenths of a magnitude unit smaller. How anyone wins under that scenario is not explained.\u003c/p>\n\u003cp>After a few days, more and better journalists weighed in. Some of them had actually studied the \u003cem>Nature\u003c/em> paper (as I have). Many, including \u003cem>Discovery News\u003c/em>'s Tim Wall, \u003ca href=\"http://news.discovery.com/earth/smaller-salton-sea-silences-seismic-shocks-110629.html\">apparently did not\u003c/a>. \u003cem>USA Today\u003c/em>'s Dan Vergano \u003ca href=\"http://content.usatoday.com/communities/sciencefair/post/2011/06/salton-sea-floods-flipped-earthquake-trigger/1\">did well\u003c/a>. So did Chris Clarke \u003ca href=\"http://www.kcet.org/updaily/socal_focus/commentary/shaking-the-salton-sea-34796.html\">on KCET's website\u003c/a>. Charles Q. Choi \u003ca href=\"http://www.ouramazingplanet.com/san-andreas-earthquake-lull-flood-control-salton-sea-1679/\">did fresh reporting\u003c/a>, as usual, for OurAmazingPlanet.com. \u003cem>Science News\u003c/em>'s Devin Powell wins my prize for his \u003ca href=\"http://www.sciencenews.org/view/generic/id/331864/title/Floodwaters_may_trigger_fault_motion\">succinct, factual and well-written account\u003c/a>. As you peruse the items collected by Google News \u003ca href=\"http://news.google.com/news/more?pz=1&cf=all&cf=all&ncl=d9Q1NWmuuBinVUMeuRGTi_qRYFWQM\">under a search on \"salton earthquake,\"\u003c/a> look for those items that get the details right—specifically the fact that the Salton Sea arose by mismanagement, not on purpose.\u003c/p>\n\u003cp>The Bay Area has excellent media when it comes to our own earthquakes, with seasoned staff and good support from academic and government experts. But still—if scary news comes up, look around the \u003ca href=\"http://geology.about.com/od/news/Geology_News_Sources.htm\">science mediasphere\u003c/a> and wait a few days before deciding what you think. Even better, \u003ca href=\"http://geology.about.com/od/news/a/DIY_news.htm\">track down the news at its source\u003c/a> whenever you can. Learn who to trust.\u003c/p>\n\u003cp>[ad floatright]\u003c/p>\n\u003cp> 33.3 -115.8\u003c/p>\n\n",
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"excerpt": "In Southern California an intriguing journal article turned into \"we're all gonna die\" TV stories in the space of a day. Be ready for the next time this happens in the Bay Area.",
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"title": "Is the Salton Sea really "15 Months Pregnant" with our next big quake? | KQED",
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"headline": "Is the Salton Sea really "15 Months Pregnant" with our next big quake?",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltontop1.jpg\" alt=\"lake cahuilla\" class=\"alignleft size-full\">\u003cem>\u003csup>The carbonate crust called tufa coats a high boulder over the Salton Sea, testifying that the Colorado River fed mighty Lake Cahuilla there in the geologically recent past. Photo by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Geologic research is a remote and dusty undertaking that can look tedious to most people. But if it bears on subjects we fear, like earthquakes, even painstaking background projects can be blown out of proportion. A recent example from Southern California went from an intriguing journal article to \"we're all gonna die\" TV stories in the space of a day. Maybe it will help you spot the next time this happens in the Bay Area.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The article, published in the prestigious \u003ci>Nature Geoscience\u003c/i> on June 26, presented the fruits of years of heat and tedium on the foul waters of the Salton Sea, in southernmost California. The Salton Sea occupies a sinking basin, the Salton Trough, that would rather be part of the Sea of Cortez except that the Colorado River has built a delta that dams it dry. As the river wanders over its delta, draining sometimes south and sometimes north, it periodically creates a geologically temporary lake in the Salton basin that has filled and dried out many times in the last few million years. (\u003ca href=\"http://www.youtube.com/watch?v=4RHu2h5CF9s\">A short video\u003c/a> by the University of Redlands illustrates the process.) \u003c/p>\n\u003cp>The repeating lake is known as Lake Cahuilla, and the Salton Sea is today's version of it. The Salton Sea is actually a terrible blunder, formed in 1905 when an irrigation canal tapping the Colorado River burst its banks and flooded a huge area of farmland in the dry bed of Lake Cahuilla. The breach was eventually fixed before the reborn lake could drown everything from Mexicali to Indio, but floods continued to be a problem until Hoover Dam was built upstream 30 years later.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The Salton Sea covers up the southern end of the San Andreas fault, and that's where our science story begins. A research team from Scripps Institution of Oceanography crisscrossed the drowned land in a small boat with a state-of-the-art CHIRP sonar system. They mapped a swarm of short faults running from the end of the San Andreas toward the end of the Imperial fault lying to the south—a tectonic configuration called a stepover. Here's the figure showing how it all fits together.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltonmap1.gif\" alt=\"salton sea tectonics\">\u003cbr>\n\u003csub>Tectonic setting of the Salton Trough and Salton Sea. SJF is San Jacinto fault, SSAF is southern San Andreas fault and IF is Imperial fault. Green grid is ship tracks in the dashed box; awz (acoustic wipeout zone) marks disturbed sediments. (Scripps)\u003c/sub>\u003c/p>\n\u003cp>From their sonar database the researchers extracted a decent record of recent ruptures on some of these stepover faults. My figure below shows, schematically, how the sediment record is built as downdrops on the fault combine with sediment being deposited on top. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/saltonprofiles1.gif\" alt=\"fault offset sediment record\">\u003c/p>\n\u003cp>The researchers ran this process backward to reconstruct the history of faulting for a few thousand years into the past.\u003c/p>\n\u003cp>What made things interesting was how this record of stepover quakes meshed with records of lake floods and San Andreas mega-quakes. The correlation is imperfect, but intriguing: every time the lake was reborn in a flood, the stepover faults gave way, and half of the recent mega-quakes coincided with stepover quakes. To connect the dots further, the researchers said that \"at least one of the last three dry-basin floods coincides with an earthquake on the SSAF (southern San Andreas fault).\" In their cautious words, \"We propose that loading by (Lake Cahuilla) may have induced failure on faults beneath the Salton Sea that, in turn, has the potential to trigger an earthquake rupture on the SSAF.\"\u003c/p>\n\u003cp>That's all ingenious science (seismic oceanography, in the desert!), but not news. To get news takes a press officer with a nose for a hook, and the hook is that the SSAF hasn't broken in some 300 years when we might (given the recent record) expect it to happen more often. Has our failure to let Lake Cahuilla be reborn held off triggering the next Big One? Well, has it?? \u003c/p>\n\u003cp>That question is something for geologists to wave their arms about at meetings and parties, not hold out to the world as a sure thing. But between the paper, \u003ca href=\"http://www.nature.com/ngeo/journal/vaop/ncurrent/full/ngeo1184.html\">whose abstract is world-readable\u003c/a>, and the \u003ca href=\"http://www.eurekalert.org/pub_releases/2011-06/uoc--foa062411.php\">press release from Scripps\u003c/a> we can see the story begin to morph. It's a scattershot press release, meant to serve any news angle, that immediately confuses today's managed Salton Sea with wild prehistoric Lake Cahuilla. It includes a great hook, a quote about the \"overdue\" SSAF likening it to \"a woman who is 15 months pregnant.\" The quote is only part of the background to the science, just a tangential part of the paper itself, but irresistible to the troutlike mind of the news reporter.\u003c/p>\n\u003cp>First out the chute on June 26 was \u003ca href=\"http://www.signonsandiego.com/news/2011/jun/26/salton-sea-poses-big-earthquake-threat-southern-ca/\">the \u003cem>San Diego Union-Tribune\u003c/em>'s website\u003c/a>, where Gary Robbins immediately removed all scientific uncertainty in his first sentence: \"The Salton Sea east of San Diego is a deceptively dangerous backwater, hiding faults that repeatedly produce powerful earthquakes that jolt all of Southern California, says a new study by the Scripps Institution of Oceanography.\" \u003c/p>\n\u003cp>Later that day a Los Angeles TV station rewrote Robbins's story under the headline \"\u003ca href=\"http://www.nbclosangeles.com/news/local/River-Diversions-could-lead-to-Megaquake-124595454.html\">Mega Quake Around the Corner?\u003c/a>\" with the lead sentence, \"Man's interference with Colorado River floods that used to regularly flow to the Salton Sea may have 'stopped the clock' on a regular series of big earthquakes, setting the stage for a mega quake that could wreck Southern California, scientists said Sunday.\" The accidental flood of 1905 has become \"interference\" with regular flows to the Salton Sea, and the reasoning has turned upside-down: If we had let the Imperial Valley drown, Southern California's \"Big One\" might already have happened and been a few tenths of a magnitude unit smaller. How anyone wins under that scenario is not explained.\u003c/p>\n\u003cp>After a few days, more and better journalists weighed in. Some of them had actually studied the \u003cem>Nature\u003c/em> paper (as I have). Many, including \u003cem>Discovery News\u003c/em>'s Tim Wall, \u003ca href=\"http://news.discovery.com/earth/smaller-salton-sea-silences-seismic-shocks-110629.html\">apparently did not\u003c/a>. \u003cem>USA Today\u003c/em>'s Dan Vergano \u003ca href=\"http://content.usatoday.com/communities/sciencefair/post/2011/06/salton-sea-floods-flipped-earthquake-trigger/1\">did well\u003c/a>. So did Chris Clarke \u003ca href=\"http://www.kcet.org/updaily/socal_focus/commentary/shaking-the-salton-sea-34796.html\">on KCET's website\u003c/a>. Charles Q. Choi \u003ca href=\"http://www.ouramazingplanet.com/san-andreas-earthquake-lull-flood-control-salton-sea-1679/\">did fresh reporting\u003c/a>, as usual, for OurAmazingPlanet.com. \u003cem>Science News\u003c/em>'s Devin Powell wins my prize for his \u003ca href=\"http://www.sciencenews.org/view/generic/id/331864/title/Floodwaters_may_trigger_fault_motion\">succinct, factual and well-written account\u003c/a>. As you peruse the items collected by Google News \u003ca href=\"http://news.google.com/news/more?pz=1&cf=all&cf=all&ncl=d9Q1NWmuuBinVUMeuRGTi_qRYFWQM\">under a search on \"salton earthquake,\"\u003c/a> look for those items that get the details right—specifically the fact that the Salton Sea arose by mismanagement, not on purpose.\u003c/p>\n\u003cp>The Bay Area has excellent media when it comes to our own earthquakes, with seasoned staff and good support from academic and government experts. But still—if scary news comes up, look around the \u003ca href=\"http://geology.about.com/od/news/Geology_News_Sources.htm\">science mediasphere\u003c/a> and wait a few days before deciding what you think. Even better, \u003ca href=\"http://geology.about.com/od/news/a/DIY_news.htm\">track down the news at its source\u003c/a> whenever you can. Learn who to trust.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"disqusTitle": "Geological Outings Around the Bay: Stinson Beach",
"title": "Geological Outings Around the Bay: Stinson Beach",
"headTitle": "QUEST | KQED Science",
"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsontop2.jpg\" alt=\"stinson beach\" class=\"alignleft size-full\">\u003cem>\u003csup>If you can tear your eyes off the sea and sky, Stinson Beach offers a geological feast in its sediments, rocks and structure. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches: it's small enough to thoroughly explore but large enough to take up a day, it offers shelter and plenty of wildlife, it has nearby places to eat and drink, and feels far from the workaday world without being a huge deal to get to.\u003c/p>\n\u003cp>But with me, geology is always a factor. Let's take in the scene.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson12.jpg\" alt=\"stinson beach view\">\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Stinson Beach is on Route 1 just north of San Francisco. You can drive there or take a bus, but either way what you see as you come in from the south is a lovely arc of sand. In the distance is the Point Reyes Peninsula with the low tableland of Bolinas on the left (a wave-cut platform) and the highlands of Point Reyes on the right. All of that land is on the Pacific plate and lies across the San Andreas fault. The fault runs just offshore, touching land in the center distance at the end of the beach and exiting the photo at upper right. Have a look at the geologic map.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\" width=\"500\" alt=\"geologic map\">\u003c/a>\u003c/p>\n\u003cp>\u003csub>Click the map for a larger version. Abbreviations: mt, marine terrace, Tms, Tertiary (Miocene) sedimentary rocks; QTs, Pliocene-Pleistocene sedimentary rocks; Kfs, Franciscan sandstone; sp, serpentinite; fc, Franciscan chert; ls, landslide deposits. From \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Marin_County.kmz\">Marin County section\u003c/a> (KMZ file) of the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/details.html\">Bay Area Geologic Map\u003c/a>.\u003c/sub>\u003c/p>\n\u003cp>Everything on the east side of the fault belongs to the Franciscan Complex, a big, sloppy geologic unit that includes bodies of sandstone, chert, shale, volcanic rocks and serpentinite. Parts of it are so mixed up that geologists have thrown up their hands and called it melange (\u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">which I featured in this post\u003c/a>).\u003c/p>\n\u003cp>If you're drawn to that great plate boundary, walk to the north end of the beach. The waves hit the beach here at an angle, sweeping the sand into crosshatches.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson22.jpg\" alt=\"sand waves\">\u003c/p>\n\u003cp>At the end of the beach is a tidal waterway leading to Bolinas Lagoon. There the repetitive wash of the tides builds symmetrical ripples like this.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson32.jpg\" alt=\"ripples\">\u003c/p>\n\u003cp>You won't see the fault here unless it happens to rupture while you're visiting, which is extremely unlikely. But if that happens, take pictures because the waves will swiftly erase the evidence. The lagoon is a feeding ground for all sorts of seabirds as well as the town's sheltered anchorage.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson42.jpg\" alt=\"bolinas lagoon\">\u003c/p>\n\u003cp>As you head south back down the beach, notice the terrace at the base of the hills, where many residences in the town of Stinson Beach sit. This is probably the same type of wave-cut platform that appears up and down the California coast (like \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a>).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson52.jpg\" alt=\"wave-cut platform\">\u003c/p>\n\u003cp>The beach's south end is a pile of boulders that have eroded from the geological plum-pudding of the Franciscan melange. The distant peninsula is the toe of an ancient landslide, one of many in this shaken-and-stirred area.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson62.jpg\" alt=\"boulders\">\u003c/p>\n\u003cp>Some of the boulders are straightforward rocks with a single composition, while others like this one are themselves melanges of many different ingredients.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson72.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>Close up, you may be able to pick out every rock type found in the Franciscan—assembled in a single boulder!\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson82.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>If you visited the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">rocks of the Marin Headlands\u003c/a> a few weeks earlier, you'll recognize the Franciscan ribbon chert here, too, although it's green rather than red. That is due to the low-grade metamorphism that has affected the entire Franciscan in most of Marin.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson92.jpg\" alt=\"green chert\">\u003c/p>\n\u003cp>While you're studying these rocks, take a look at the cliff behind them, which is an intimate mixture of rocks and matrix that keeps crumbling into the waves to yield Stinson Beach's abundance of fresh, dark sand. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson992.jpg\" alt=\"folded chert\">\u003c/p>\n\u003cp>I always stay til sundown.\u003c/p>\n\u003cp>What are your top Bay Area beaches, and why?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.899 -122.645\u003c/p>\n\n",
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"excerpt": "Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches. But with me, geology is always a factor. Let's take in the scene.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsontop2.jpg\" alt=\"stinson beach\" class=\"alignleft size-full\">\u003cem>\u003csup>If you can tear your eyes off the sea and sky, Stinson Beach offers a geological feast in its sediments, rocks and structure. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches: it's small enough to thoroughly explore but large enough to take up a day, it offers shelter and plenty of wildlife, it has nearby places to eat and drink, and feels far from the workaday world without being a huge deal to get to.\u003c/p>\n\u003cp>But with me, geology is always a factor. Let's take in the scene.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson12.jpg\" alt=\"stinson beach view\">\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Stinson Beach is on Route 1 just north of San Francisco. You can drive there or take a bus, but either way what you see as you come in from the south is a lovely arc of sand. In the distance is the Point Reyes Peninsula with the low tableland of Bolinas on the left (a wave-cut platform) and the highlands of Point Reyes on the right. All of that land is on the Pacific plate and lies across the San Andreas fault. The fault runs just offshore, touching land in the center distance at the end of the beach and exiting the photo at upper right. Have a look at the geologic map.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\" width=\"500\" alt=\"geologic map\">\u003c/a>\u003c/p>\n\u003cp>\u003csub>Click the map for a larger version. Abbreviations: mt, marine terrace, Tms, Tertiary (Miocene) sedimentary rocks; QTs, Pliocene-Pleistocene sedimentary rocks; Kfs, Franciscan sandstone; sp, serpentinite; fc, Franciscan chert; ls, landslide deposits. From \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Marin_County.kmz\">Marin County section\u003c/a> (KMZ file) of the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/details.html\">Bay Area Geologic Map\u003c/a>.\u003c/sub>\u003c/p>\n\u003cp>Everything on the east side of the fault belongs to the Franciscan Complex, a big, sloppy geologic unit that includes bodies of sandstone, chert, shale, volcanic rocks and serpentinite. Parts of it are so mixed up that geologists have thrown up their hands and called it melange (\u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">which I featured in this post\u003c/a>).\u003c/p>\n\u003cp>If you're drawn to that great plate boundary, walk to the north end of the beach. The waves hit the beach here at an angle, sweeping the sand into crosshatches.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson22.jpg\" alt=\"sand waves\">\u003c/p>\n\u003cp>At the end of the beach is a tidal waterway leading to Bolinas Lagoon. There the repetitive wash of the tides builds symmetrical ripples like this.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson32.jpg\" alt=\"ripples\">\u003c/p>\n\u003cp>You won't see the fault here unless it happens to rupture while you're visiting, which is extremely unlikely. But if that happens, take pictures because the waves will swiftly erase the evidence. The lagoon is a feeding ground for all sorts of seabirds as well as the town's sheltered anchorage.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson42.jpg\" alt=\"bolinas lagoon\">\u003c/p>\n\u003cp>As you head south back down the beach, notice the terrace at the base of the hills, where many residences in the town of Stinson Beach sit. This is probably the same type of wave-cut platform that appears up and down the California coast (like \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a>).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson52.jpg\" alt=\"wave-cut platform\">\u003c/p>\n\u003cp>The beach's south end is a pile of boulders that have eroded from the geological plum-pudding of the Franciscan melange. The distant peninsula is the toe of an ancient landslide, one of many in this shaken-and-stirred area.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson62.jpg\" alt=\"boulders\">\u003c/p>\n\u003cp>Some of the boulders are straightforward rocks with a single composition, while others like this one are themselves melanges of many different ingredients.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson72.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>Close up, you may be able to pick out every rock type found in the Franciscan—assembled in a single boulder!\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson82.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>If you visited the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">rocks of the Marin Headlands\u003c/a> a few weeks earlier, you'll recognize the Franciscan ribbon chert here, too, although it's green rather than red. That is due to the low-grade metamorphism that has affected the entire Franciscan in most of Marin.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson92.jpg\" alt=\"green chert\">\u003c/p>\n\u003cp>While you're studying these rocks, take a look at the cliff behind them, which is an intimate mixture of rocks and matrix that keeps crumbling into the waves to yield Stinson Beach's abundance of fresh, dark sand. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson992.jpg\" alt=\"folded chert\">\u003c/p>\n\u003cp>I always stay til sundown.\u003c/p>\n\u003cp>What are your top Bay Area beaches, and why?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.899 -122.645\u003c/p>\n\n\u003c/div>\u003c/p>",
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"disqusTitle": "Geological Outings Around the Bay: The Cordelia and Green Valley Faults",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliaflttop2.jpg\" alt=\"cordelia fault\" class=\"alignleft size-full\">\u003cem>\u003csup>The Cordelia fault, west of Fairfield, provides the best exposure of the San Andreas fault zone in the Bay Area. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>The San Andreas fault is called the boundary between the North American and Pacific plates. It gets a lot of attention, but the plate-tectonic action actually is spread over a wide band of active faults on both sides, west and east, of the San Andreas proper. The easternmost strand of the San Andreas fault zone lies in Napa and Solano counties. This simple road trip will get you acquainted with it.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The textbooks say that the thin bright line of the San Andreas fault is the plate boundary, but in real life the North American plate is deeply splintered halfway to the Rockies. North America and the Pacific have about 2 inches a year of motion between them. The San Andreas proper accounts for the majority of that, but lesser faults in the Coast Range like the Hayward, Calaveras, Rodgers Creek and Maacama take up a large share too. Even the crustal cracks east of the Sierra Nevada move a few millimeters a year. Basically, the whole Bay Area sits within the plate boundary.\u003c/p>\n\u003cp>Around here, the easternmost part of that boundary consists of the Greenville/Concord fault in the East Bay and the Green Valley fault in the North Bay. The two faults are considered to be connected, although they are offset a few kilometers from each other beneath Suisun Bay. Both are worth a day trip, but let's go north this time. Here's a look at the geology of the area between Fairfield and Napa.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/greenvlyfltmap2.jpg\" width=\"500\" alt=\"geologic map\">\u003cbr>\n\u003csub>\u003cem>From the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Napa_County.kmz\">Napa County geologic map\u003c/a> and \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Solano_County.kmz\">Solano County geologic map\u003c/a> in Google Earth—click for 750-pixel version\u003c/em>\u003c/sub>\u003c/p>\n\u003cp>The purple area is young lavas and related rocks of the Sonoma Volcanics. The green area is much older sedimentary rocks of the Great Valley Sequence; we won't see those. The gold in between is widespread \u003ca href=\"http://ww2.kqed.org/quest/2011/03/31/landslide-season/\">landslide deposits\u003c/a>.\u003c/p>\n\u003cp>We'll start west of Fairfield at the Green Valley Road exit from I-80 eastbound, which is just before the intersection with I-680. From 680 take exit 70 and take three right turns to reach Lopes Road, which becomes Green Valley Road. Now the fun part begins as you make your leisurely way into Green Valley. The valley is bounded along its west side by the Green Valley fault, which runs north into private land in the rugged hills. The Green Valley fault seems to rupture every thousand years or so (and last ruptured between 1600 and 1800), but there isn't much data. There is some \u003ca href=\"http://ww2.kqed.org/quest/2011/05/05/geological-outings-around-the-bay-a-visit-to-the-hayward-fault/\">creep motion\u003c/a> measured on it.\u003c/p>\n\u003cp>The Green Valley fault is not easily visited, but its smaller sibling is—the Cordelia fault. It runs through the lava hills on the east side of Green Valley. About 3.5 miles up Green Valley Road, Rockville Road exits to the right. Take it over the hills for about a mile and a half until you reach a dramatic roadcut. This is it looking west from the far side. On the geologic map above, it's at the north end of the Cordelia fault.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltcut2.jpg\" alt=\"cordelia fault roadcut\">\u003c/p>\n\u003cp>Pull over and find the distinct trace of the fault, made obvious where the finely ground rock, or gouge, in the fault zone has crumbled out.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltgouge2.jpg\" alt=\"cordelia fault trace\">\u003c/p>\n\u003cp>The west side of the Cordelia fault is moving north, but no movement has been recorded in historic time. This is an easygoing fault, at the edge of the busy zone on the plate boundary. It's about as user-friendly as a fault can be, and its appearance here is the best fault exposure in the Bay Area.\u003c/p>\n\u003cp>Take the time to inspect the rocks, too. Take a sample if you like. These are volcanic rocks—not lava flows, but tuff: hot-welded bodies of ash and other volcano stuff laid down in huge burning avalanches back when this region was an eruptive center. (\u003ca href=\"http://ww2.kqed.org/quest/2011/04/28/bay-area-volcanoes/\">Today Clear Lake and The Geysers is the center of activity.\u003c/a>)\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltrocks2.jpg\" alt=\"sonoma volcanics\">\u003cbr>\n\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltclast2.jpg\" alt=\"tuff clast\">\u003c/p>\n\u003cp>In a few places you'll find welded tuff, an assemblage of an intriguing variety of material that has cooked together into a sturdy stone. (\u003ca href=\"http://geology.about.com/od/more_igrocks/ig/extrusives/weldtuffcloseup.htm\">Here's a closeup.\u003c/a>)\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliaflttuff2.jpg\" alt=\"sonoma volcanics welded tuff\">\u003c/p>\n\u003cp>If you have the time, just a little farther there's an entrance to Fairfield's \u003ca href=\"http://www.fairfield.ca.gov/gov/depts/pw/open_space/rockville_hills_regional_park/default.asp\">Rockville Hills Regional Park\u003c/a> and an \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?wp=GC2418F\">EarthCache\u003c/a> connected to the Cordelia fault.\u003c/p>\n\u003cp>From here, continue on Rockville Road and turn left on Suisun Valley Road. This leads into the hills and becomes Wooden Valley Road. After about a 10-mile drive you'll enter the charming Wooden Valley, at the top center of the geologic map. From there you can look west to the Green Valley fault again as it emerges from the hills and runs along a high scarp. The fault ends just north of here.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/GVFnorthend2.jpg\" alt=\"green valley fault\">\u003c/p>\n\u003cp>Wooden Valley Road ends at state route 121, Monticello Road. Turn left on it and drive along the Green Valley fault. Notice the \u003ca href=\"http://geology.about.com/od/naturalhazardsclimate/ig/Landslides/woodenvlydebrisflow.htm\">landslide scar from 2006\u003c/a> in the picture above and watch for it as you drive past; the whole hillside is unstable. Where the road turns sharply right and heads into the woods, there's a small turnout where you can admire the view east over Wooden Valley to the highest spot in this part of the Coast Range, Blue Ridge topped by Mount Vaca. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/GVFnorthview2.jpg\" alt=\"view from green valley fault\">\u003c/p>\n\u003cp>From here it's a nice drive through the volcanic hills down to Napa and the heart of the wine country.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 38.2538 -122.1395\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliaflttop2.jpg\" alt=\"cordelia fault\" class=\"alignleft size-full\">\u003cem>\u003csup>The Cordelia fault, west of Fairfield, provides the best exposure of the San Andreas fault zone in the Bay Area. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>The San Andreas fault is called the boundary between the North American and Pacific plates. It gets a lot of attention, but the plate-tectonic action actually is spread over a wide band of active faults on both sides, west and east, of the San Andreas proper. The easternmost strand of the San Andreas fault zone lies in Napa and Solano counties. This simple road trip will get you acquainted with it.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The textbooks say that the thin bright line of the San Andreas fault is the plate boundary, but in real life the North American plate is deeply splintered halfway to the Rockies. North America and the Pacific have about 2 inches a year of motion between them. The San Andreas proper accounts for the majority of that, but lesser faults in the Coast Range like the Hayward, Calaveras, Rodgers Creek and Maacama take up a large share too. Even the crustal cracks east of the Sierra Nevada move a few millimeters a year. Basically, the whole Bay Area sits within the plate boundary.\u003c/p>\n\u003cp>Around here, the easternmost part of that boundary consists of the Greenville/Concord fault in the East Bay and the Green Valley fault in the North Bay. The two faults are considered to be connected, although they are offset a few kilometers from each other beneath Suisun Bay. Both are worth a day trip, but let's go north this time. Here's a look at the geology of the area between Fairfield and Napa.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/greenvlyfltmap2.jpg\" width=\"500\" alt=\"geologic map\">\u003cbr>\n\u003csub>\u003cem>From the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Napa_County.kmz\">Napa County geologic map\u003c/a> and \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Solano_County.kmz\">Solano County geologic map\u003c/a> in Google Earth—click for 750-pixel version\u003c/em>\u003c/sub>\u003c/p>\n\u003cp>The purple area is young lavas and related rocks of the Sonoma Volcanics. The green area is much older sedimentary rocks of the Great Valley Sequence; we won't see those. The gold in between is widespread \u003ca href=\"http://ww2.kqed.org/quest/2011/03/31/landslide-season/\">landslide deposits\u003c/a>.\u003c/p>\n\u003cp>We'll start west of Fairfield at the Green Valley Road exit from I-80 eastbound, which is just before the intersection with I-680. From 680 take exit 70 and take three right turns to reach Lopes Road, which becomes Green Valley Road. Now the fun part begins as you make your leisurely way into Green Valley. The valley is bounded along its west side by the Green Valley fault, which runs north into private land in the rugged hills. The Green Valley fault seems to rupture every thousand years or so (and last ruptured between 1600 and 1800), but there isn't much data. There is some \u003ca href=\"http://ww2.kqed.org/quest/2011/05/05/geological-outings-around-the-bay-a-visit-to-the-hayward-fault/\">creep motion\u003c/a> measured on it.\u003c/p>\n\u003cp>The Green Valley fault is not easily visited, but its smaller sibling is—the Cordelia fault. It runs through the lava hills on the east side of Green Valley. About 3.5 miles up Green Valley Road, Rockville Road exits to the right. Take it over the hills for about a mile and a half until you reach a dramatic roadcut. This is it looking west from the far side. On the geologic map above, it's at the north end of the Cordelia fault.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltcut2.jpg\" alt=\"cordelia fault roadcut\">\u003c/p>\n\u003cp>Pull over and find the distinct trace of the fault, made obvious where the finely ground rock, or gouge, in the fault zone has crumbled out.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltgouge2.jpg\" alt=\"cordelia fault trace\">\u003c/p>\n\u003cp>The west side of the Cordelia fault is moving north, but no movement has been recorded in historic time. This is an easygoing fault, at the edge of the busy zone on the plate boundary. It's about as user-friendly as a fault can be, and its appearance here is the best fault exposure in the Bay Area.\u003c/p>\n\u003cp>Take the time to inspect the rocks, too. Take a sample if you like. These are volcanic rocks—not lava flows, but tuff: hot-welded bodies of ash and other volcano stuff laid down in huge burning avalanches back when this region was an eruptive center. (\u003ca href=\"http://ww2.kqed.org/quest/2011/04/28/bay-area-volcanoes/\">Today Clear Lake and The Geysers is the center of activity.\u003c/a>)\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltrocks2.jpg\" alt=\"sonoma volcanics\">\u003cbr>\n\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliafltclast2.jpg\" alt=\"tuff clast\">\u003c/p>\n\u003cp>In a few places you'll find welded tuff, an assemblage of an intriguing variety of material that has cooked together into a sturdy stone. (\u003ca href=\"http://geology.about.com/od/more_igrocks/ig/extrusives/weldtuffcloseup.htm\">Here's a closeup.\u003c/a>)\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/cordeliaflttuff2.jpg\" alt=\"sonoma volcanics welded tuff\">\u003c/p>\n\u003cp>If you have the time, just a little farther there's an entrance to Fairfield's \u003ca href=\"http://www.fairfield.ca.gov/gov/depts/pw/open_space/rockville_hills_regional_park/default.asp\">Rockville Hills Regional Park\u003c/a> and an \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?wp=GC2418F\">EarthCache\u003c/a> connected to the Cordelia fault.\u003c/p>\n\u003cp>From here, continue on Rockville Road and turn left on Suisun Valley Road. This leads into the hills and becomes Wooden Valley Road. After about a 10-mile drive you'll enter the charming Wooden Valley, at the top center of the geologic map. From there you can look west to the Green Valley fault again as it emerges from the hills and runs along a high scarp. The fault ends just north of here.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/GVFnorthend2.jpg\" alt=\"green valley fault\">\u003c/p>\n\u003cp>Wooden Valley Road ends at state route 121, Monticello Road. Turn left on it and drive along the Green Valley fault. Notice the \u003ca href=\"http://geology.about.com/od/naturalhazardsclimate/ig/Landslides/woodenvlydebrisflow.htm\">landslide scar from 2006\u003c/a> in the picture above and watch for it as you drive past; the whole hillside is unstable. Where the road turns sharply right and heads into the woods, there's a small turnout where you can admire the view east over Wooden Valley to the highest spot in this part of the Coast Range, Blue Ridge topped by Mount Vaca. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/GVFnorthview2.jpg\" alt=\"view from green valley fault\">\u003c/p>\n\u003cp>From here it's a nice drive through the volcanic hills down to Napa and the heart of the wine country.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 38.2538 -122.1395\u003c/p>\n\n\u003c/div>\u003c/p>",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/sloanebook.jpg\" alt=\"geology lecture\" class=\"alignleft size-full\">\u003cem>\u003csup>Doris Sloane, author of Geology of the San Francisco Bay Region, gives a public lecture in the Berkeley Hills in 2007. Photo by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Learning about geology isn't just a matter of going out and wandering around, as fun as that is. Books help a lot, starting with a simple rocks-and-minerals guide. Going beyond that first book can lead to a library, and my own shelves keep getting more crowded. Books for Bay Area geology enthusiasts make up a more manageable list. Let me show you my favorites.\u003cbr>\n\u003c!--more-->\u003c/p>\n\u003cp>I have reviewed several of these for About.com. To see those reviews, click the asterisk next to the book title.\u003c/p>\n\u003cp>\u003cstrong>Appetizers\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003cem>California Rocks!\u003c/em>\u003c/strong>, by Katherine Baylor (Mountain Press), is an appetite-whetting collection of 65 geo-destinations around the state, 14 of them in the Bay Area. Photo-licious and engaging, this is a book to pull out whether you're planning a California vacation or a local day trip.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Roadside Geology of Northern and Central California\u003c/em>\u003c/strong>, by David Alt and Donald Hyndman (Mountain Press), covers wider ground and is organized around the major roads. It's an excellent companion for any California road trip, giving you insight into the landscape around your windshield and suggestions for side trips when you have an extra hour or two.\u003c/p>\n\u003cp>\u003cstrong>Entrees\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003ci>Geology of the San Francisco Bay Region\u003c/i> \u003ca href=\"http://geology.about.com/od/bookreviews/fr/booksloan.htm\">*\u003c/a>\u003c/strong>, by Doris Sloane with photographs by John Karachewsky (UC Press), is a beautifully produced compendium that systematically introduces the region from the Bay itself to the mountains around it, including maps, tables of information, field trip ideas and the background knowledge to make the most of them. It's built to last, too.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>A Streetcar to Subduction\u003c/em>\u003c/strong>, by the late Clyde Wahrhaftig (American Geophysical Union), presents seven field trips in and near San Francisco using public transit. Wahrhaftig, who never learned to drive, was a superb field geologist and teacher.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Field Guide to the San Andreas Fault\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/gr/lynchSAFguide.htm\">*\u003c/a>\u003c/strong>, by David Lynch (Thule Scientific), is a mile-by-mile road log that covers the great fault from end to end. If you're as serious about the fault as I am, you'll want this to support the extensive traveling it will take to visit the whole thing. It's divided into 12 day trips, three of which encompass the Bay Area.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Finding Fault in California: An Earthquake Tourist's Guide\u003c/em> \u003ca href=\"http://geology.about.com/msubbook.htm\">*\u003c/a>\u003c/strong>, by Susan Hough (Mountain Press), focuses on faults throughout California that you can visit in person, but the San Andreas naturally has pride of place. Hough is a very good teacher of earthquake science, too.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Geologic Field Trips in Northern California\u003c/em>\u003c/strong> (California Division of Mines and Geology Special Publication 119) is a hard-core set of annotated road logs published for the Geological Society of America's Cordilleran Section centennial meeting in 1999. Trips include unsung features in the Bay Area and outliers such as the Sutter Buttes, Santa Lucia Range and the western Sierra.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>1906 San Francisco Earthquake Centennial Field Guides\u003c/em>\u003c/strong> (Geological Society of America Field Guide 7) includes annotated walks in San Francisco, day trips in the surrounding area, and \u003ca href=\"http://geology.about.com/od/geophoto_tours/ig/CAtransecttrip/\">a four-day loop through Northern California\u003c/a> exploring subduction rocks.\u003c/p>\n\u003cp>\u003cstrong>Dessert\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Magnitude 8\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/fr/fradkinmag8.htm\">*\u003c/a>\u003c/strong>, by Philip Fradkin (UC Press), is my favorite book on the San Andreas fault for home reading because Fradkin goes beyond geology and field trips (which he covers well) to explore the mindset that our earthquake-prone region has fostered. There is no better treatment of the geologic roots of our peculiar local culture.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>A Wine Journey along the Russian River\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/gr/heimoffwine.htm\">*\u003c/a>\u003c/strong>, by Steve Heimoff (UC Press), explores the land and vines and wines associated with the Russian River. It's naturally a treat for wine lovers, but he treats the river itself and the rocks it traverses in unexpected depth. If wine is your magic key to everything else, this will open a new door for you.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>San Francisco Bay\u003c/em>\u003c/strong>, by Harold Gilliam (Doubleday), is a 1957 classic that will smother you in pleasure and nostalgia as it sweeps through the geological, natural and cultural history of \"California's vital inland sea.\" Look for it wherever old books are sold.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Day Trips: Roaming the Backroads of Northern California\u003c/em>\u003c/strong>, by Peter Browning (Chronicle Books), is a supplementary text that will help you reach some truly remote parts of the Bay Area, although it will not tell you a lot about the rocks you're seeing.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Rocks and Minerals of California\u003c/em>\u003c/strong>, by Vinson Brown, David Allan and James Stark (Naturegraph), is a compact guide to mineral localities of the whole state. It includes abundant maps and tables that will get you to places no other book will list.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.7749295 -122.4194155\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/sloanebook.jpg\" alt=\"geology lecture\" class=\"alignleft size-full\">\u003cem>\u003csup>Doris Sloane, author of Geology of the San Francisco Bay Region, gives a public lecture in the Berkeley Hills in 2007. Photo by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Learning about geology isn't just a matter of going out and wandering around, as fun as that is. Books help a lot, starting with a simple rocks-and-minerals guide. Going beyond that first book can lead to a library, and my own shelves keep getting more crowded. Books for Bay Area geology enthusiasts make up a more manageable list. Let me show you my favorites.\u003cbr>\n\u003c!--more-->\u003c/p>\n\u003cp>I have reviewed several of these for About.com. To see those reviews, click the asterisk next to the book title.\u003c/p>\n\u003cp>\u003cstrong>Appetizers\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003cem>California Rocks!\u003c/em>\u003c/strong>, by Katherine Baylor (Mountain Press), is an appetite-whetting collection of 65 geo-destinations around the state, 14 of them in the Bay Area. Photo-licious and engaging, this is a book to pull out whether you're planning a California vacation or a local day trip.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Roadside Geology of Northern and Central California\u003c/em>\u003c/strong>, by David Alt and Donald Hyndman (Mountain Press), covers wider ground and is organized around the major roads. It's an excellent companion for any California road trip, giving you insight into the landscape around your windshield and suggestions for side trips when you have an extra hour or two.\u003c/p>\n\u003cp>\u003cstrong>Entrees\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003ci>Geology of the San Francisco Bay Region\u003c/i> \u003ca href=\"http://geology.about.com/od/bookreviews/fr/booksloan.htm\">*\u003c/a>\u003c/strong>, by Doris Sloane with photographs by John Karachewsky (UC Press), is a beautifully produced compendium that systematically introduces the region from the Bay itself to the mountains around it, including maps, tables of information, field trip ideas and the background knowledge to make the most of them. It's built to last, too.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>A Streetcar to Subduction\u003c/em>\u003c/strong>, by the late Clyde Wahrhaftig (American Geophysical Union), presents seven field trips in and near San Francisco using public transit. Wahrhaftig, who never learned to drive, was a superb field geologist and teacher.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Field Guide to the San Andreas Fault\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/gr/lynchSAFguide.htm\">*\u003c/a>\u003c/strong>, by David Lynch (Thule Scientific), is a mile-by-mile road log that covers the great fault from end to end. If you're as serious about the fault as I am, you'll want this to support the extensive traveling it will take to visit the whole thing. It's divided into 12 day trips, three of which encompass the Bay Area.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Finding Fault in California: An Earthquake Tourist's Guide\u003c/em> \u003ca href=\"http://geology.about.com/msubbook.htm\">*\u003c/a>\u003c/strong>, by Susan Hough (Mountain Press), focuses on faults throughout California that you can visit in person, but the San Andreas naturally has pride of place. Hough is a very good teacher of earthquake science, too.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Geologic Field Trips in Northern California\u003c/em>\u003c/strong> (California Division of Mines and Geology Special Publication 119) is a hard-core set of annotated road logs published for the Geological Society of America's Cordilleran Section centennial meeting in 1999. Trips include unsung features in the Bay Area and outliers such as the Sutter Buttes, Santa Lucia Range and the western Sierra.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>1906 San Francisco Earthquake Centennial Field Guides\u003c/em>\u003c/strong> (Geological Society of America Field Guide 7) includes annotated walks in San Francisco, day trips in the surrounding area, and \u003ca href=\"http://geology.about.com/od/geophoto_tours/ig/CAtransecttrip/\">a four-day loop through Northern California\u003c/a> exploring subduction rocks.\u003c/p>\n\u003cp>\u003cstrong>Dessert\u003c/strong>\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Magnitude 8\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/fr/fradkinmag8.htm\">*\u003c/a>\u003c/strong>, by Philip Fradkin (UC Press), is my favorite book on the San Andreas fault for home reading because Fradkin goes beyond geology and field trips (which he covers well) to explore the mindset that our earthquake-prone region has fostered. There is no better treatment of the geologic roots of our peculiar local culture.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>A Wine Journey along the Russian River\u003c/em> \u003ca href=\"http://geology.about.com/od/bookreviews/gr/heimoffwine.htm\">*\u003c/a>\u003c/strong>, by Steve Heimoff (UC Press), explores the land and vines and wines associated with the Russian River. It's naturally a treat for wine lovers, but he treats the river itself and the rocks it traverses in unexpected depth. If wine is your magic key to everything else, this will open a new door for you.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>San Francisco Bay\u003c/em>\u003c/strong>, by Harold Gilliam (Doubleday), is a 1957 classic that will smother you in pleasure and nostalgia as it sweeps through the geological, natural and cultural history of \"California's vital inland sea.\" Look for it wherever old books are sold.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Day Trips: Roaming the Backroads of Northern California\u003c/em>\u003c/strong>, by Peter Browning (Chronicle Books), is a supplementary text that will help you reach some truly remote parts of the Bay Area, although it will not tell you a lot about the rocks you're seeing.\u003c/p>\n\u003cp>\u003cstrong>\u003cem>Rocks and Minerals of California\u003c/em>\u003c/strong>, by Vinson Brown, David Allan and James Stark (Naturegraph), is a compact guide to mineral localities of the whole state. 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"disqusTitle": "Mount Diablo Views",
"title": "Mount Diablo Views",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablo300.jpg\" alt=\"mount diablo\" class=\"alignleft size-full\">\u003cem>\u003csup>Mount Diablo is seen with its foothills from Wildcat Canyon Road near Inspiration Point in the Berkeley Hills. Photo courtesy \u003ca href=\"http://www.flickr.com/photos/hortulus_aptus/\">Seán O'Hara\u003c/a> of Flickr under Creative commons license. Photos by Andrew Alden unless otherwise indicated.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Mount Diablo, in the heart of the East Bay, is an interesting mountain in many ways. It has fossils. It has a lot of serpentinite in it, with the accompanying \u003ca href=\"http://ww2.kqed.org/quest/2010/08/16/home-sweet-serpentine/\">serpentine plant community\u003c/a>. It's been mined for mercury and other metals. It's an exceptional structure even in a region of crazy-complicated tectonic structures. But I expect to get into the geological details some other time. Because first of all, Mount Diablo is just \u003ci>there\u003c/i>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>Mount Diablo was always a landmark, so widely visible around the Bay and central California that in 1851 its peak was named the base line for land divisions. Around here and across the majority of California and all of Nevada, every \u003ca href=\"http://geology.about.com/od/maps/ig/township-range/\">township and section\u003c/a> is numbered in relation to the north-south Mt. Diablo Meridian and the east-west Mt. Diablo Base Line. (Full details are given by the \u003ca href=\"http://www.mdshs.org/\">Mount Diablo Surveyors Historical Society\u003c/a>.)\u003c/p>\n\u003cp>Today few of us have any awareness of land division, and we can simply enjoy the peak's prominence as we drive Bay Area roads or hike the hills. Around the Bay proper, Mount Diablo peeks over the Berkeley Hills as seen from Corona Heights in San Francisco . . .\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosf.jpg\" alt=\"mount diablo san francisco\">\u003c/p>\n\u003cp>. . . or from the hills above Marin City, where the \"devil's mountain\" overlooks Angel Island.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiabloangel.jpg\" alt=\"angel island\">\u003c/p>\n\u003cp>To see the peak's full extent we need to cross the hills of the East Bay, or at least climb them. Here the mountain is seen from the Los Buellis Hills, east of San Jose, looking up the valley formed by the Calaveras fault.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosanjose.jpg\" alt=\"mount diablo san jose\">\u003c/p>\n\u003cp>Once over the hills, your every vista centers around Diablo whether it's the view from Oakland . . .\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosiesta.jpg\" alt=\"mount diablo siesta valley\">\u003c/p>\n\u003cp>. . . or from the Tassajara Valley . . .\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablotassa.jpg\" alt=\"tassajara valley\">\u003c/p>\n\u003cp>. . . or from the Delta:\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosjv.jpg\" alt=\"delta\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/philosophygeek/\">Mark Johnson\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>On Interstate 5, Mount Diablo can be spotted from the Dunnigan Hills in the north to near Patterson in the south. From state route 99 it's visible from a much longer stretch, but only if the conditions are right. In fact, instead of driving everywhere to determine Mount Diablo's viewshed, it's more efficient to visit the peak itself on a perfect day and look outward. There's a handy sign pointing out what's possible on a perfect day.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosign.jpg\" alt=\"mount diablo sign\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/allaboutgeorge/\">George Kelly\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>I've been up there on a perfect day, and while it's not geometrically possible, atmospheric refraction has allowed me to spot Mount Shasta. An example of a typical excellent (not perfect) day shows Pyramid Peak in the central Sierra Nevada.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosierra.jpg\" alt=\"sierra nevada\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/people/14657061@N00/\">advencap\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>Such days were once more common. A. J. McCall, standing at the Sierra's crest on September 7, 1849, recorded \"a picture of wonderful grandeur and magnificence\":\u003c/p>\n\u003cblockquote>\n\u003cp>\"Below were a succession of innumerable pine-covered mountain peaks, growing less and less until they disappeared in a broad, yellow valley sweeping north and south until lost to view, and beyond another range of mountains. This was the far-famed Sacramento Valley, nearly a hundred miles distant. The purity of the atmosphere rendered vision almost illimitable, showing every line and shadow distinctly.\" (\u003ca href=\"http://geology.about.com/b/2010/03/19/hard-road-west-by-keith-meldahl.htm\">source\u003c/a>)\u003c/p>\n\u003c/blockquote>\n\u003cp>Today the activities of ten million modern Californians make such purity almost unattainable—especially around Labor Day.\u003c/p>\n\u003cp>There's a common belief that when pioneer scout Kit Carson guided the Fremont Expedition over the Sierra in the winter of 1844 (at today's Carson Pass), he recognized his position by spotting Mount Diablo: \"There is the little mountain—it is 15 years since I saw it; but I am just as sure as if I had seen it yesterday.\" But \u003ca href=\"http://www.longcamp.com/little_mountain.html\">Bob Graham and Peter Lathrop argue convincingly\u003c/a> that it was not Diablo, but the whole Coast Range that Carson meant. That's too bad; it was a good story.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.8817 -121.9146\u003c/p>\n\n",
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"excerpt": "Mount Diablo, in the heart of the East Bay, is an interesting mountain in many ways. But first of all, Mount Diablo is just \u003ci>there\u003c/i>.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablo300.jpg\" alt=\"mount diablo\" class=\"alignleft size-full\">\u003cem>\u003csup>Mount Diablo is seen with its foothills from Wildcat Canyon Road near Inspiration Point in the Berkeley Hills. Photo courtesy \u003ca href=\"http://www.flickr.com/photos/hortulus_aptus/\">Seán O'Hara\u003c/a> of Flickr under Creative commons license. Photos by Andrew Alden unless otherwise indicated.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Mount Diablo, in the heart of the East Bay, is an interesting mountain in many ways. It has fossils. It has a lot of serpentinite in it, with the accompanying \u003ca href=\"http://ww2.kqed.org/quest/2010/08/16/home-sweet-serpentine/\">serpentine plant community\u003c/a>. It's been mined for mercury and other metals. It's an exceptional structure even in a region of crazy-complicated tectonic structures. But I expect to get into the geological details some other time. Because first of all, Mount Diablo is just \u003ci>there\u003c/i>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>Mount Diablo was always a landmark, so widely visible around the Bay and central California that in 1851 its peak was named the base line for land divisions. Around here and across the majority of California and all of Nevada, every \u003ca href=\"http://geology.about.com/od/maps/ig/township-range/\">township and section\u003c/a> is numbered in relation to the north-south Mt. Diablo Meridian and the east-west Mt. Diablo Base Line. (Full details are given by the \u003ca href=\"http://www.mdshs.org/\">Mount Diablo Surveyors Historical Society\u003c/a>.)\u003c/p>\n\u003cp>Today few of us have any awareness of land division, and we can simply enjoy the peak's prominence as we drive Bay Area roads or hike the hills. Around the Bay proper, Mount Diablo peeks over the Berkeley Hills as seen from Corona Heights in San Francisco . . .\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosf.jpg\" alt=\"mount diablo san francisco\">\u003c/p>\n\u003cp>. . . or from the hills above Marin City, where the \"devil's mountain\" overlooks Angel Island.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiabloangel.jpg\" alt=\"angel island\">\u003c/p>\n\u003cp>To see the peak's full extent we need to cross the hills of the East Bay, or at least climb them. Here the mountain is seen from the Los Buellis Hills, east of San Jose, looking up the valley formed by the Calaveras fault.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosanjose.jpg\" alt=\"mount diablo san jose\">\u003c/p>\n\u003cp>Once over the hills, your every vista centers around Diablo whether it's the view from Oakland . . .\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosiesta.jpg\" alt=\"mount diablo siesta valley\">\u003c/p>\n\u003cp>. . . or from the Tassajara Valley . . .\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablotassa.jpg\" alt=\"tassajara valley\">\u003c/p>\n\u003cp>. . . or from the Delta:\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosjv.jpg\" alt=\"delta\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/philosophygeek/\">Mark Johnson\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>On Interstate 5, Mount Diablo can be spotted from the Dunnigan Hills in the north to near Patterson in the south. From state route 99 it's visible from a much longer stretch, but only if the conditions are right. In fact, instead of driving everywhere to determine Mount Diablo's viewshed, it's more efficient to visit the peak itself on a perfect day and look outward. There's a handy sign pointing out what's possible on a perfect day.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosign.jpg\" alt=\"mount diablo sign\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/allaboutgeorge/\">George Kelly\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>I've been up there on a perfect day, and while it's not geometrically possible, atmospheric refraction has allowed me to spot Mount Shasta. An example of a typical excellent (not perfect) day shows Pyramid Peak in the central Sierra Nevada.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/mtdiablosierra.jpg\" alt=\"sierra nevada\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/people/14657061@N00/\">advencap\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>Such days were once more common. A. J. McCall, standing at the Sierra's crest on September 7, 1849, recorded \"a picture of wonderful grandeur and magnificence\":\u003c/p>\n\u003cblockquote>\n\u003cp>\"Below were a succession of innumerable pine-covered mountain peaks, growing less and less until they disappeared in a broad, yellow valley sweeping north and south until lost to view, and beyond another range of mountains. This was the far-famed Sacramento Valley, nearly a hundred miles distant. The purity of the atmosphere rendered vision almost illimitable, showing every line and shadow distinctly.\" (\u003ca href=\"http://geology.about.com/b/2010/03/19/hard-road-west-by-keith-meldahl.htm\">source\u003c/a>)\u003c/p>\n\u003c/blockquote>\n\u003cp>Today the activities of ten million modern Californians make such purity almost unattainable—especially around Labor Day.\u003c/p>\n\u003cp>There's a common belief that when pioneer scout Kit Carson guided the Fremont Expedition over the Sierra in the winter of 1844 (at today's Carson Pass), he recognized his position by spotting Mount Diablo: \"There is the little mountain—it is 15 years since I saw it; but I am just as sure as if I had seen it yesterday.\" But \u003ca href=\"http://www.longcamp.com/little_mountain.html\">Bob Graham and Peter Lathrop argue convincingly\u003c/a> that it was not Diablo, but the whole Coast Range that Carson meant. That's too bad; it was a good story.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.8817 -121.9146\u003c/p>\n\n\u003c/div>\u003c/p>",
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"content": "\u003cp>In 2005, a partial skeleton of a juvenile mammoth was discovered along the Guadalupe River near downtown San Jose. A full-scale replica is now featured in a new exhibit at the Children's Discovery Museum in San Jose. Learn more with Kaitlin Maguire from the UC Museum of Paleontology about these majestic creatures that roamed the Bay Area during the Ice Age .\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\u003cp>\u003c/p>\n",
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"disqusTitle": "New Fossils from the Caldecott Tunnel",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecotthorsemolar3002.jpg\" alt=\"caldecot tunnel fossils\" class=\"alignleft size-full\">\u003cem>\u003csup>\"Paleo mitigation\" work during the dig of the new Caldecott Tunnel bore has yielded fresh insight into a familiar set of rocks thanks to fossils like this Miocene horse molar. All photos courtesy CalTrans and PaleoResource Consultants.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>The fourth bore for the Caldecott Tunnel, which connects Oakland and points west with Orinda and points east, is being dug day and night with the first drive-throughs slated for 2013. Part of the job is what Caltrans contracts call \"\u003ca href=\"http://www.dot.ca.gov/hq/env/paleo/index.htm\">paleontological mitigation\u003c/a>\": allowing fossil scientists to salvage resources—\"fossils and the deposits they are found in\"—that would otherwise be destroyed. A paleo mitigation agreement governs the Caldecott fourth bore project, and scientists shared some of the early results earlier this month.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>Fossil hunting is tedious, exacting work, but there are those who love it. Kristin McCallister, a paleontologist for contractor \u003ca href=\"http://www.paleoresource.com/\">PaleoResource\u003c/a>, is shown here during early work at the job site, examining spoils.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottKristinMcCallister2.jpg\" alt=\"paleontologist\">\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The vast majority of fossils are microscopic and consist of plankton or pollen grains. But the big bones are sexy. Let's look at the pictures PaleoResource's Lanny Fisk showed at the \u003ca href=\"http://paleoresource.com/calpaleo.html\">CalPaleo 2011 meeting\u003c/a> in Rocklin, starting with the leg bone of a rhinoceros.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottrhinolegorinda2.jpg\" alt=\"caldecott rhino\">\u003c/p>\n\u003cp>Here are two vertebrae of a Miocene camel species.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottcamelvertorinda2.jpg\" alt=\"caldecott camel\">\u003c/p>\n\u003cp>And this is the metatarsal bone of an ancient horse.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecotthoresemetatarsorinda2.jpg\" alt=\"caldecott horse\">\u003c/p>\n\u003cp>Finally here's the upper jaw of an \u003ca href=\"http://en.wikipedia.org/wiki/Oreodont\">oreodont\u003c/a>, an extinct browsing mammal the size of a sheep.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottoreodontjaworinda2.jpg\" alt=\"caldecott oreodont\">\u003c/p>\n\u003cp>All of these (plus bird, pronghorn and wolverine bones) were salvaged from rocks of the Orinda Formation that are about 11 million years old, a time late in the Miocene Epoch. The researchers also found hundreds of plant fossils for the first time in these rocks, including this laurel leaf.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottlaurelorinda2.jpg\" alt=\"caldecott laurel\">\u003c/p>\n\u003cp>The Orinda Formation makes up the eastern end of the bore. In the middle is the \u003ca href=\"http://oaklandgeology.wordpress.com/2008/04/06/claremont-chert-close-up/\">Claremont Formation\u003c/a>, a cherty unit that holds up the highest part of the Berkeley Hills. This 1-inch clam is from the Claremont.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottclamclaremont2.jpg\" alt=\"caldecott clam\">\u003c/p>\n\u003cp>Obviously this shows a change from a land to a sea environment as we go back in time. \u003c/p>\n\u003cp>At the west end of the bore is the still older Sobrante Formation. Fisk told the CalPaleo audience that this unit has yielded a large fish fossil fauna as well as some leaves and marine invertebrates (clams, crabs and plankton). He was particularly excited about the fish, which somewhat resemble cool-water fish of this age from northwestern Oregon.\u003c/p>\n\u003cp>One handicap that Fisk mentioned was difficulty getting into the tunnel, where paleontologists can watch the rock face and stop operations long enough to examine and salvage the best fossils. Working the spoils pile isn't good for getting exact locations and geological context for fossils. But the bore will be carried out in two passes, and maybe we can get another look at this unique dig.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.858 -122.214\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecotthorsemolar3002.jpg\" alt=\"caldecot tunnel fossils\" class=\"alignleft size-full\">\u003cem>\u003csup>\"Paleo mitigation\" work during the dig of the new Caldecott Tunnel bore has yielded fresh insight into a familiar set of rocks thanks to fossils like this Miocene horse molar. All photos courtesy CalTrans and PaleoResource Consultants.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>The fourth bore for the Caldecott Tunnel, which connects Oakland and points west with Orinda and points east, is being dug day and night with the first drive-throughs slated for 2013. Part of the job is what Caltrans contracts call \"\u003ca href=\"http://www.dot.ca.gov/hq/env/paleo/index.htm\">paleontological mitigation\u003c/a>\": allowing fossil scientists to salvage resources—\"fossils and the deposits they are found in\"—that would otherwise be destroyed. A paleo mitigation agreement governs the Caldecott fourth bore project, and scientists shared some of the early results earlier this month.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>Fossil hunting is tedious, exacting work, but there are those who love it. Kristin McCallister, a paleontologist for contractor \u003ca href=\"http://www.paleoresource.com/\">PaleoResource\u003c/a>, is shown here during early work at the job site, examining spoils.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottKristinMcCallister2.jpg\" alt=\"paleontologist\">\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The vast majority of fossils are microscopic and consist of plankton or pollen grains. But the big bones are sexy. Let's look at the pictures PaleoResource's Lanny Fisk showed at the \u003ca href=\"http://paleoresource.com/calpaleo.html\">CalPaleo 2011 meeting\u003c/a> in Rocklin, starting with the leg bone of a rhinoceros.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottrhinolegorinda2.jpg\" alt=\"caldecott rhino\">\u003c/p>\n\u003cp>Here are two vertebrae of a Miocene camel species.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottcamelvertorinda2.jpg\" alt=\"caldecott camel\">\u003c/p>\n\u003cp>And this is the metatarsal bone of an ancient horse.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecotthoresemetatarsorinda2.jpg\" alt=\"caldecott horse\">\u003c/p>\n\u003cp>Finally here's the upper jaw of an \u003ca href=\"http://en.wikipedia.org/wiki/Oreodont\">oreodont\u003c/a>, an extinct browsing mammal the size of a sheep.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottoreodontjaworinda2.jpg\" alt=\"caldecott oreodont\">\u003c/p>\n\u003cp>All of these (plus bird, pronghorn and wolverine bones) were salvaged from rocks of the Orinda Formation that are about 11 million years old, a time late in the Miocene Epoch. The researchers also found hundreds of plant fossils for the first time in these rocks, including this laurel leaf.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottlaurelorinda2.jpg\" alt=\"caldecott laurel\">\u003c/p>\n\u003cp>The Orinda Formation makes up the eastern end of the bore. In the middle is the \u003ca href=\"http://oaklandgeology.wordpress.com/2008/04/06/claremont-chert-close-up/\">Claremont Formation\u003c/a>, a cherty unit that holds up the highest part of the Berkeley Hills. This 1-inch clam is from the Claremont.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/caldecottclamclaremont2.jpg\" alt=\"caldecott clam\">\u003c/p>\n\u003cp>Obviously this shows a change from a land to a sea environment as we go back in time. \u003c/p>\n\u003cp>At the west end of the bore is the still older Sobrante Formation. Fisk told the CalPaleo audience that this unit has yielded a large fish fossil fauna as well as some leaves and marine invertebrates (clams, crabs and plankton). He was particularly excited about the fish, which somewhat resemble cool-water fish of this age from northwestern Oregon.\u003c/p>\n\u003cp>One handicap that Fisk mentioned was difficulty getting into the tunnel, where paleontologists can watch the rock face and stop operations long enough to examine and salvage the best fossils. Working the spoils pile isn't good for getting exact locations and geological context for fossils. But the bore will be carried out in two passes, and maybe we can get another look at this unique dig.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.858 -122.214\u003c/p>\n\n\u003c/div>\u003c/p>",
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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnthumb2.jpg\" alt=\"ring mountain view\">\u003cem>\u003csup>Ring Mountain invites the eyes outward with superb views of the Bay, but looking down at its rocks is also a rewarding pleasure. All photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>California is known among geologists as a type locality for subduction. In everyday language this means a place that exposes textbook-quality examples of subduction-related rocks and tectonic features. The rarest and most scientifically precious of these is in Tiburon, and part of it is on pristine display at \u003ca href=\"http://www.maringov.org/en/Depts/PK/Divisions/Open%20Space/Ring%20Mountain.aspx\">Ring Mountain Open Space Preserve\u003c/a>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>I've shown you some subduction-related localities in previous posts: Deep seafloor in the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands\u003c/a>, pelagic limestone \u003ca href=\"http://ww2.kqed.org/quest/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">in Pacifica\u003c/a>, and melange at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a> on the Sonoma coast all represent the upper parts of subduction complexes. Ring Mountain lets us peek downward into their hellish depths.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The body of rock underlying the central Tiburon Peninsula is part of the large and sprawling Franciscan Complex, an assemblage of materials that was once involved in subduction. The oceanic plate whose small remnant is the Juan de Fuca plate, off Cascadia, has been subducting under North America for many millions of years. Most Franciscan rock is ordinary sandstone and shale, laid down offshore, that has been crushed and crunched in the subduction zone. Volcanic rocks on and in the oceanic crust are mixed in with these. The Ring Mountain block actually went deep down the subduction zone and somehow came back out. Thus it's a high-grade block, one that underwent a high degree of metamorphism. A large portion of it is serpentinite, yielding the typical toxic soil of a serpentine barren.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtntamview2.jpg\" alt=\"ring mountain serpentine\">\u003c/p>\n\u003cp>Amid that matrix is a large number of rocks bearing the signs of extremely deep burial recorded in their minerals. These have unfamiliar names like glaucophane, lawsonite, jadeite and actinolite. Together, they indicate very high pressure but relatively low temperature (specifically, pressures up to 2.5 GPa and temperatures of about 550°C). The ensemble is called blueschist, shown here.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnblueschist2.jpg\" alt=\"blueschist\">\u003c/p>\n\u003cp>The pressure corresponds to depths around 100 kilometers, but this is not a straightforward matter and the depths could be less than half that. The tale the minerals tell is one in which cold volcanic rocks of the seafloor were carried down quickly to these depths, not fully heating up. There the rocks were metamorphosed into a new set of high-pressure, low-temperature minerals. Then somehow the rocks returned with comparable speed to the surface, so that these minerals could not change back to their original species. (This \u003ca href=\"http://geology.about.com/library/bl/images/blretrometamorph.htm\">retrograde metamorphism\u003c/a> is why these minerals so rarely occur in surface rocks.) The rocks emerge totally changed.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnboulder2.jpg\" alt=\"ring mountain serpentinite\">\u003c/p>\n\u003cp>The picture this conjures up is that of a packet of rocks being spat out of the subduction zone like a watermelon seed in the fingers. But geologists don't accept stories because they seem sensible; they use them as scenarios to test over and over against the rocks. That's where the conversation among the specialists sits today.\u003c/p>\n\u003cp>Ring Mountain is many other things to its visitors. Rock climbers like the bouldering and may not notice the streamlined shapes that resulted from the kneading action in the subduction zone.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnrock2.jpg\" alt=\"bouldering\">\u003c/p>\n\u003cp>Botanists love the flowers and plants endemic to the serpentine habitat.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnflower2.jpg\" alt=\"ring mountain flower\">\u003c/p>\n\u003cp>Photographers love Ring Mountain because it offers everything from the large scale to the small, with an endless variety of light and subjects. If you go, take only pictures because every rock and plant is protected there.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtncloseup2.jpg\" alt=\"ring mountain stone\">\u003c/p>\n\u003cp>Find out more about Ring Mountain's geology on \"\u003ca href=\"http://www.marin.edu/~jim/ring/index.html\">To See A World from Ring Mountain\u003c/a>\" by Jim Locke of the College of Marin.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.909 -122.491\u003c/p>\n\n",
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"excerpt": "The body of rock underlying the central Tiburon Peninsula is the rarest and most scientifically precious part of the Franciscan Complex, an assemblage of materials that was once involved in subduction.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnthumb2.jpg\" alt=\"ring mountain view\">\u003cem>\u003csup>Ring Mountain invites the eyes outward with superb views of the Bay, but looking down at its rocks is also a rewarding pleasure. All photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>California is known among geologists as a type locality for subduction. In everyday language this means a place that exposes textbook-quality examples of subduction-related rocks and tectonic features. The rarest and most scientifically precious of these is in Tiburon, and part of it is on pristine display at \u003ca href=\"http://www.maringov.org/en/Depts/PK/Divisions/Open%20Space/Ring%20Mountain.aspx\">Ring Mountain Open Space Preserve\u003c/a>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>I've shown you some subduction-related localities in previous posts: Deep seafloor in the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands\u003c/a>, pelagic limestone \u003ca href=\"http://ww2.kqed.org/quest/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">in Pacifica\u003c/a>, and melange at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a> on the Sonoma coast all represent the upper parts of subduction complexes. Ring Mountain lets us peek downward into their hellish depths.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The body of rock underlying the central Tiburon Peninsula is part of the large and sprawling Franciscan Complex, an assemblage of materials that was once involved in subduction. The oceanic plate whose small remnant is the Juan de Fuca plate, off Cascadia, has been subducting under North America for many millions of years. Most Franciscan rock is ordinary sandstone and shale, laid down offshore, that has been crushed and crunched in the subduction zone. Volcanic rocks on and in the oceanic crust are mixed in with these. The Ring Mountain block actually went deep down the subduction zone and somehow came back out. Thus it's a high-grade block, one that underwent a high degree of metamorphism. A large portion of it is serpentinite, yielding the typical toxic soil of a serpentine barren.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtntamview2.jpg\" alt=\"ring mountain serpentine\">\u003c/p>\n\u003cp>Amid that matrix is a large number of rocks bearing the signs of extremely deep burial recorded in their minerals. These have unfamiliar names like glaucophane, lawsonite, jadeite and actinolite. Together, they indicate very high pressure but relatively low temperature (specifically, pressures up to 2.5 GPa and temperatures of about 550°C). The ensemble is called blueschist, shown here.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnblueschist2.jpg\" alt=\"blueschist\">\u003c/p>\n\u003cp>The pressure corresponds to depths around 100 kilometers, but this is not a straightforward matter and the depths could be less than half that. The tale the minerals tell is one in which cold volcanic rocks of the seafloor were carried down quickly to these depths, not fully heating up. There the rocks were metamorphosed into a new set of high-pressure, low-temperature minerals. Then somehow the rocks returned with comparable speed to the surface, so that these minerals could not change back to their original species. (This \u003ca href=\"http://geology.about.com/library/bl/images/blretrometamorph.htm\">retrograde metamorphism\u003c/a> is why these minerals so rarely occur in surface rocks.) The rocks emerge totally changed.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnboulder2.jpg\" alt=\"ring mountain serpentinite\">\u003c/p>\n\u003cp>The picture this conjures up is that of a packet of rocks being spat out of the subduction zone like a watermelon seed in the fingers. But geologists don't accept stories because they seem sensible; they use them as scenarios to test over and over against the rocks. That's where the conversation among the specialists sits today.\u003c/p>\n\u003cp>Ring Mountain is many other things to its visitors. Rock climbers like the bouldering and may not notice the streamlined shapes that resulted from the kneading action in the subduction zone.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnrock2.jpg\" alt=\"bouldering\">\u003c/p>\n\u003cp>Botanists love the flowers and plants endemic to the serpentine habitat.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtnflower2.jpg\" alt=\"ring mountain flower\">\u003c/p>\n\u003cp>Photographers love Ring Mountain because it offers everything from the large scale to the small, with an endless variety of light and subjects. If you go, take only pictures because every rock and plant is protected there.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/05/ringmtncloseup2.jpg\" alt=\"ring mountain stone\">\u003c/p>\n\u003cp>Find out more about Ring Mountain's geology on \"\u003ca href=\"http://www.marin.edu/~jim/ring/index.html\">To See A World from Ring Mountain\u003c/a>\" by Jim Locke of the College of Marin.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.909 -122.491\u003c/p>\n\n\u003c/div>\u003c/p>",
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"source": "kqed",
"order": 8
},
"link": "/californiareport",
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},
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"id": "californiareportmagazine",
"title": "The California Report Magazine",
"tagline": "Your state, your stories",
"info": "Every week, The California Report Magazine takes you on a road trip for the ears: to visit the places and meet the people who make California unique. The in-depth storytelling podcast from the California Report.",
"airtime": "FRI 4:30pm-5pm, 6:30pm-7pm, 11pm-11:30pm",
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"order": 10
},
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM3NjkwNjk1OTAz",
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},
"city-arts": {
"id": "city-arts",
"title": "City Arts & Lectures",
"info": "A one-hour radio program to hear celebrated writers, artists and thinkers address contemporary ideas and values, often discussing the creative process. Please note: tapes or transcripts are not available",
"imageSrc": "https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/05/cityartsandlecture-300x300.jpg",
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"airtime": "SUN 1pm-2pm, TUE 10pm, WED 1am",
"meta": {
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"source": "City Arts & Lectures"
},
"link": "https://www.cityarts.net",
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"rss": "https://www.cityarts.net/feed/"
}
},
"closealltabs": {
"id": "closealltabs",
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"order": 1
},
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"title": "Code Switch / Life Kit",
"info": "\u003cem>Code Switch\u003c/em>, which listeners will hear in the first part of the hour, has fearless and much-needed conversations about race. Hosted by journalists of color, the show tackles the subject of race head-on, exploring how it impacts every part of society — from politics and pop culture to history, sports and more.\u003cbr />\u003cbr />\u003cem>Life Kit\u003c/em>, which will be in the second part of the hour, guides you through spaces and feelings no one prepares you for — from finances to mental health, from workplace microaggressions to imposter syndrome, from relationships to parenting. The show features experts with real world experience and shares their knowledge. Because everyone needs a little help being human.\u003cbr />\u003cbr />\u003ca href=\"https://www.npr.org/podcasts/510312/codeswitch\">\u003cem>Code Switch\u003c/em> offical site and podcast\u003c/a>\u003cbr />\u003ca href=\"https://www.npr.org/lifekit\">\u003cem>Life Kit\u003c/em> offical site and podcast\u003c/a>\u003cbr />",
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"id": "commonwealth-club",
"title": "Commonwealth Club of California Podcast",
"info": "The Commonwealth Club of California is the nation's oldest and largest public affairs forum. As a non-partisan forum, The Club brings to the public airwaves diverse viewpoints on important topics. The Club's weekly radio broadcast - the oldest in the U.S., dating back to 1924 - is carried across the nation on public radio stations and is now podcasting. Our website archive features audio of our recent programs, as well as selected speeches from our long and distinguished history. This podcast feed is usually updated twice a week and is always un-edited.",
"airtime": "THU 10pm, FRI 1am",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Commonwealth-Club-Podcast-Tile-360x360-1.jpg",
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"source": "Commonwealth Club of California"
},
"link": "/radio/program/commonwealth-club",
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"google": "https://podcasts.google.com/feed/aHR0cDovL3d3dy5jb21tb253ZWFsdGhjbHViLm9yZy9hdWRpby9wb2RjYXN0L3dlZWtseS54bWw",
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},
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"id": "forum",
"title": "Forum",
"tagline": "The conversation starts here",
"info": "KQED’s live call-in program discussing local, state, national and international issues, as well as in-depth interviews.",
"airtime": "MON-FRI 9am-11am, 10pm-11pm",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Forum-Podcast-Tile-703x703-1.jpg",
"imageAlt": "KQED Forum with Mina Kim and Alexis Madrigal",
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"source": "kqed",
"order": 9
},
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM5NTU3MzgxNjMz",
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"imageSrc": "https://ww2.kqed.org/news/wp-content/uploads/sites/10/2018/05/freakonomicsRadio.png",
"officialWebsiteLink": "http://freakonomics.com/",
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"meta": {
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"source": "WNYC"
},
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"apple": "https://itunes.apple.com/us/podcast/freakonomics-radio/id354668519",
"tuneIn": "https://tunein.com/podcasts/WNYC-Podcasts/Freakonomics-Radio-p272293/",
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},
"fresh-air": {
"id": "fresh-air",
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"apple": "https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=214089682&at=11l79Y&ct=nprdirectory",
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"here-and-now": {
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"info": "A live production of NPR and WBUR Boston, in collaboration with stations across the country, Here & Now reflects the fluid world of news as it's happening in the middle of the day, with timely, in-depth news, interviews and conversation. Hosted by Robin Young, Jeremy Hobson and Tonya Mosley.",
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"rss": "https://feeds.npr.org/510051/podcast.xml"
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},
"hidden-brain": {
"id": "hidden-brain",
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"info": "Shankar Vedantam uses science and storytelling to reveal the unconscious patterns that drive human behavior, shape our choices and direct our relationships.",
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"airtime": "SUN 7pm-8pm",
"meta": {
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"source": "NPR"
},
"link": "/radio/program/hidden-brain",
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},
"how-i-built-this": {
"id": "how-i-built-this",
"title": "How I Built This with Guy Raz",
"info": "Guy Raz dives into the stories behind some of the world's best known companies. How I Built This weaves a narrative journey about innovators, entrepreneurs and idealists—and the movements they built.",
"imageSrc": "https://ww2.kqed.org/news/wp-content/uploads/sites/10/2018/05/howIBuiltThis.png",
"officialWebsiteLink": "https://www.npr.org/podcasts/510313/how-i-built-this",
"airtime": "SUN 7:30pm-8pm",
"meta": {
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"source": "npr"
},
"link": "/radio/program/how-i-built-this",
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"npr": "https://rpb3r.app.goo.gl/3zxy",
"apple": "https://itunes.apple.com/us/podcast/how-i-built-this-with-guy-raz/id1150510297?mt=2",
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},
"hyphenacion": {
"id": "hyphenacion",
"title": "Hyphenación",
"tagline": "Where conversation and cultura meet",
"info": "What kind of no sabo word is Hyphenación? For us, it’s about living within a hyphenation. Like being a third-gen Mexican-American from the Texas border now living that Bay Area Chicano life. Like Xorje! Each week we bring together a couple of hyphenated Latinos to talk all about personal life choices: family, careers, relationships, belonging … everything is on the table. ",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2025/03/Hyphenacion_FinalAssets_PodcastTile.png",
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"officialWebsiteLink": "/podcasts/hyphenacion",
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"order": 15
},
"link": "/podcasts/hyphenacion",
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"spotify": "https://open.spotify.com/show/2p3Fifq96nw9BPcmFdIq0o?si=39209f7b25774f38",
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"rss": "https://feeds.megaphone.fm/KQINC2275451163"
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},
"jerrybrown": {
"id": "jerrybrown",
"title": "The Political Mind of Jerry Brown",
"tagline": "Lessons from a lifetime in politics",
"info": "The Political Mind of Jerry Brown brings listeners the wisdom of the former Governor, Mayor, and presidential candidate. Scott Shafer interviewed Brown for more than 40 hours, covering the former governor's life and half-century in the political game and Brown has some lessons he'd like to share. ",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/The-Political-Mind-of-Jerry-Brown-Podcast-Tile-703x703-1.jpg",
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"officialWebsiteLink": "/podcasts/jerrybrown",
"meta": {
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"source": "kqed",
"order": 18
},
"link": "/podcasts/jerrybrown",
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"apple": "https://itunes.apple.com/us/podcast/id1492194549",
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}
},
"latino-usa": {
"id": "latino-usa",
"title": "Latino USA",
"airtime": "MON 1am-2am, SUN 6pm-7pm",
"info": "Latino USA, the radio journal of news and culture, is the only national, English-language radio program produced from a Latino perspective.",
"imageSrc": "https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/04/latinoUsa.jpg",
"officialWebsiteLink": "http://latinousa.org/",
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},
"link": "/radio/program/latino-usa",
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"apple": "https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=79681317&at=11l79Y&ct=nprdirectory",
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"rss": "https://feeds.npr.org/510016/podcast.xml"
}
},
"marketplace": {
"id": "marketplace",
"title": "Marketplace",
"info": "Our flagship program, helmed by Kai Ryssdal, examines what the day in money delivered, through stories, conversations, newsworthy numbers and more. Updated Monday through Friday at about 3:30 p.m. PT.",
"airtime": "MON-FRI 4pm-4:30pm, MON-WED 6:30pm-7pm",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Marketplace-Podcast-Tile-360x360-1.jpg",
"officialWebsiteLink": "https://www.marketplace.org/",
"meta": {
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"source": "American Public Media"
},
"link": "/radio/program/marketplace",
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"rss": "https://feeds.publicradio.org/public_feeds/marketplace-pm/rss/rss"
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},
"masters-of-scale": {
"id": "masters-of-scale",
"title": "Masters of Scale",
"info": "Masters of Scale is an original podcast in which LinkedIn co-founder and Greylock Partner Reid Hoffman sets out to describe and prove theories that explain how great entrepreneurs take their companies from zero to a gazillion in ingenious fashion.",
"airtime": "Every other Wednesday June 12 through October 16 at 8pm (repeats Thursdays at 2am)",
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"meta": {
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"source": "WaitWhat"
},
"link": "/radio/program/masters-of-scale",
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"rss": "https://rss.art19.com/masters-of-scale"
}
},
"mindshift": {
"id": "mindshift",
"title": "MindShift",
"tagline": "A podcast about the future of learning and how we raise our kids",
"info": "The MindShift podcast explores the innovations in education that are shaping how kids learn. Hosts Ki Sung and Katrina Schwartz introduce listeners to educators, researchers, parents and students who are developing effective ways to improve how kids learn. We cover topics like how fed-up administrators are developing surprising tactics to deal with classroom disruptions; how listening to podcasts are helping kids develop reading skills; the consequences of overparenting; and why interdisciplinary learning can engage students on all ends of the traditional achievement spectrum. This podcast is part of the MindShift education site, a division of KQED News. KQED is an NPR/PBS member station based in San Francisco. You can also visit the MindShift website for episodes and supplemental blog posts or tweet us \u003ca href=\"https://twitter.com/MindShiftKQED\">@MindShiftKQED\u003c/a> or visit us at \u003ca href=\"/mindshift\">MindShift.KQED.org\u003c/a>",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Mindshift-Podcast-Tile-703x703-1.jpg",
"imageAlt": "KQED MindShift: How We Will Learn",
"officialWebsiteLink": "/mindshift/",
"meta": {
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"source": "kqed",
"order": 12
},
"link": "/podcasts/mindshift",
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM1NzY0NjAwNDI5",
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}
},
"morning-edition": {
"id": "morning-edition",
"title": "Morning Edition",
"info": "\u003cem>Morning Edition\u003c/em> takes listeners around the country and the world with multi-faceted stories and commentaries every weekday. Hosts Steve Inskeep, David Greene and Rachel Martin bring you the latest breaking news and features to prepare you for the day.",
"airtime": "MON-FRI 3am-9am",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Morning-Edition-Podcast-Tile-360x360-1.jpg",
"officialWebsiteLink": "https://www.npr.org/programs/morning-edition/",
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"link": "/radio/program/morning-edition"
},
"onourwatch": {
"id": "onourwatch",
"title": "On Our Watch",
"tagline": "Deeply-reported investigative journalism",
"info": "For decades, the process for how police police themselves has been inconsistent – if not opaque. In some states, like California, these proceedings were completely hidden. After a new police transparency law unsealed scores of internal affairs files, our reporters set out to examine these cases and the shadow world of police discipline. On Our Watch brings listeners into the rooms where officers are questioned and witnesses are interrogated to find out who this system is really protecting. Is it the officers, or the public they've sworn to serve?",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/On-Our-Watch-Podcast-Tile-703x703-1.jpg",
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"officialWebsiteLink": "/podcasts/onourwatch",
"meta": {
"site": "news",
"source": "kqed",
"order": 11
},
"link": "/podcasts/onourwatch",
"subscribe": {
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5ucHIub3JnLzUxMDM2MC9wb2RjYXN0LnhtbD9zYz1nb29nbGVwb2RjYXN0cw",
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}
},
"on-the-media": {
"id": "on-the-media",
"title": "On The Media",
"info": "Our weekly podcast explores how the media 'sausage' is made, casts an incisive eye on fluctuations in the marketplace of ideas, and examines threats to the freedom of information and expression in America and abroad. For one hour a week, the show tries to lift the veil from the process of \"making media,\" especially news media, because it's through that lens that we see the world and the world sees us",
"airtime": "SUN 2pm-3pm, MON 12am-1am",
"imageSrc": "https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/04/onTheMedia.png",
"officialWebsiteLink": "https://www.wnycstudios.org/shows/otm",
"meta": {
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"source": "wnyc"
},
"link": "/radio/program/on-the-media",
"subscribe": {
"apple": "https://itunes.apple.com/us/podcast/on-the-media/id73330715?mt=2",
"tuneIn": "https://tunein.com/radio/On-the-Media-p69/",
"rss": "http://feeds.wnyc.org/onthemedia"
}
},
"pbs-newshour": {
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