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"content": "\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/sunshot11.jpg\" alt=\"\">\u003cem>Jasper Ridge Biological Preserve\u003c/em>\u003c/span>\u003c/p>\n\u003cp>\u003ca href=\"http://jrbp.stanford.edu/\" target=\"_blank\">Jasper Ridge Biological Preserve\u003c/a> can easily be missed: just off Highway 280 in the city of Woodside, the entrance is blocked by a rusted metal gate with a small sign that reads 'No Tresspassing, Area Patrolled.'\u003c/p>\n\u003cp>But some of the folks at QUEST - including yours truly - got a special tour of the preserve. I joined reporter David Gorn and biologist Scott Loarie on a three hour hike around Jasper Ridge's Searsville Lake.\u003c/p>\n\u003cp>I learned that plant-life on the preserve, and most endemic California plant-life, are in trouble.\u003c/p>\n\u003cp>At least, that's what Loarie and his team at Stanford predict. \"If plants can't adapt to the climate changes,\" says Loarie, \"Then by the end of the century two-thirds of California plants face an 80 percent reduction.\"\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>So which plants are most likely to go as the global climate changes, well, the plants that have a hard time with seed dispersion. Plants like Bay Laurel, the California Buckeye, Madrone and the Western Burning Bush have seeds that aren't easily dispersed. This gives them a very concentrated zone for growth. If the climate shifts slightly in that particular region, then the these California natives could all die out.\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/laurel1.jpg\" alt=\"\">\u003cem>Bay Laurel\u003c/em>\u003c/span>\u003c/p>\n\u003cp>The plants that do have an easier time are those with a wide seed dispersion - like the beautiful but dangerous Poison Oak, the Coyote Bush, Clarkia, Virgin's Bower and Box Elder Maple. These plants all have small seeds that are easily dispersed by the wind, or by birds. By dispersing their seeds to various climates, these plants will have a better chance of surviving.\u003c/p>\n\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/virgin11.jpg\" alt=\"\">\u003cem>Virgin's Bower\u003c/em>\u003c/span>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>So which California plants will survive a century from now? It's hard to say. But what is definite is that preserves like Jasper Ridge are crucial for monitoring and protecting California's unique plant life.\u003cbr>\n\u003cbr clear=\"all\">\u003cbr>\n\u003cspan class=\"left\">\u003ca href=\"http://ww2.kqed.org/quest/audio/disappearing-plants\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/images/tv_icon_light.gif\" alt=\"\">\u003c/a>\u003c/span>View a slideshow of the\u003ca href=\"http://ww2.kqed.org/quest/audio/disappearing-plants\">\"Disappearing Plants\" Radio Report\u003c/a> online, as well as find additional links and resources.\u003cbr>\n37.404946 -122.244593\u003c/p>\n\n",
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"content": "\u003cp>It was the talk of my Wednesday morning Pilates class. \"I'm letting my lawn die, but saving the plants. Plants are harder to replace.\" \"We only lived in our house six months last year! How are we going to reduce 19 percent of nothing?\" \"We get our irrigation water from a creek.\" \"We don't have any grass.\"\u003c/p>\n\u003cp>This was in response to the East Bay Municipal Utility District (EBMUD) \u003ca href=\"http://www.ebmud.com/current_events/press_releases/Drought%20Press%20Release.pdf\" target=\"_blank\">declaring a water emergency\u003c/a> and implementing water-rationing rules, to begin August 1. Residential customers in single-family homes must cut back their water use by 19 percent compared to their average over the past three years. Apartment dwellers only have to cut back 11 percent. No washing your car without a shut-off nozzle. No washing down sidewalks or driveways, and any fountains and ponds should be filled with recycled water only.\u003c/p>\n\u003cp>Anyone who uses less than 100 gallons of water a day is off the hook. Prices for water over 100 gallons per day will increase 10 percent. Those who don't cut back at least 10 percent will have to pay $2 for every 750 gallons of water they use over that amount. EBMUD is hiring water police to patrol the neighborhoods looking for water wasters. You'll get some warnings for breaking the rules, but repeat offenders could have their water cut off.\u003c/p>\n\u003cp>For those of us who live east of the Caldecott Tunnel, cutting back almost 20 percent means that lawns will have to die. Most of our water use, on average, goes to keep landscaping alive. My wife and I are letting most of our front lawn return to desert. We will eventually have what's left of the grass torn out and replaced with native, water-sipping plants and lots and lots of mulch. (Right now landscapers are pretty busy.) Those who live west of the Caldecott will have an easier time saving water because it is on average cooler than on the east side, and lawns in places like Oakland, Berkeley, and El Cerrito are relatively small. They will have to save on indoor water use, however.\u003c/p>\n\u003cp>For help on saving water, and to find out how to get free low-flow fixtures for your home, go to the EBMUD Web site, \u003ca href=\"http://www.ebmud.com/\">www.ebmud.com\u003c/a>. There is a bonus to saving water indoors. Saving hot water by using low-flow showerheads, showering or bathing every other day, washing only full loads of dishes in your dishwasher, washing only full loads of laundry in your washing machine, and \u003ca href=\"http://ww2.kqed.org/quest/2007/04/06/cold-water-works/\" target=\"_blank\">using cold water laundry detergent\u003c/a>, will save you energy and money as well as water. For those of us who don't yet have dual-flush toilets that flush a little for number 1 and more for number 2, it's good to remember the mantra of the 1970s water crisis, \"If it's brown, flush it down. If it's yellow, let it mellow.\" You better explain that to the houseguest you host this summer from the flooded Midwest.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\u003cp>\u003c/p>\n",
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"content": "\u003cp align=\"center\">\u003cem>This Exploration created in collaboration with the \u003c/em>\u003ca href=\"http://www.exploratorium.edu\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/imp/explo_logo_black3.gif\" border=\"0\">\u003c/a>\u003c/p>\n\u003cp>\u003c!-- iframe plugin v.4.3 wordpress.org/plugins/iframe/ -->\u003cbr>\n\u003ciframe src=\"http://www.everytrail.com/guide/sibley-volcanic-regional-preserve-exploration/map?embed=true\" marginheight=\"0\" marginwidth=\"0\" frameborder=\"0\" scrolling=\"no\" width=\"980\" height=\"450\" class=\"iframe-class\">\u003c/iframe>\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003c/span>As sure as the earth moves in Oakland, there's a volcano just off Skyline Boulevard. Not just any volcano, mind you. This one's lying on its side with its guts exposed. You might not recognize it right away, owing to its reclining position and the grassy coat it's adopted. But among the shrubs and grasses at Sibley Volcanic Regional Preserve, you'll find the rocky body and underpinnings of one of the largest of a handful of volcanoes that once dotted our geologic neighborhood. Join us and naturalist Steve Edwards of the East Bay Regional Park District on our latest Bay Area science hike.\u003c/p>\n\u003ch3>Location\u003c/h3>\n\u003cp>6800 Skyline Blvd, Oakland, CA 94611 [\u003ca href=\"http://tinyurl.com/6lj4lr\">Map\u003c/a>]\u003cbr>\nPhone: 888-EBPARKS (888-327-2757), option 3, extension 4554\u003c/p>\n\u003cp>Open between 5 a.m. and 10 p.m. unless otherwise posted or permitted\u003cbr>\n\u003ca href=\"http://www.ebparks.org/parks/sibley\">Download a trail map\u003c/a> and more about the park.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cem>Special thanks to Steve Edwards, Isa Polt-Jones and Rosemary Cameron of the \u003ca href=\"http://www.ebparks.org\">East Bay Regional Parks District\u003c/a> for their participation.\u003c/em>\u003cbr>\n\u003cem>Robin Marks contributed to this Exploration.\u003c/em>\u003c/p>\n\u003ch2>Sibley's Round Top: A Sideways Volcano\u003c/h2>\n\u003ch3>Volcanoes in the East Bay? Really?\u003c/h3>\n\u003cp>\u003cspan class=\"right\">\u003cimg src=\"http://farm3.static.flickr.com/2082/2516290125_6cbb5fd770_m.jpg\" width=\"240\" height=\"161\">\u003c/span>As sure as the earth moves in Berkeley, there's a volcano just off Skyline Boulevard. Not just any volcano, mind you. This one's laying on its side with its guts exposed. You might not recognize it right away, owing to its reclining position and the grassy coat it's adopted. But among the shrubs and grasses at Sibley Regional Volcanic Preserve, you'll find the rocky body and layered underpinnings of one of the largest of a handful of volcanoes that once dotted our geologic neighborhood.\u003c/p>\n\u003cp>Ten million years ago, a vent now called Round Top sprouted in the Earth's crust and regularly spewed thick, gooey lava into its environs. At that time, Round Top stood upright, like a proper volcano, south of present-day San Jose. Over the millennia, the volcano's been ferried northward by the motion of nearby faults, a rugged journey that's changed the appearance of the mountain and the land around it.\u003c/p>\n\u003ch3>A few volcanic basics\u003c/h3>\n\u003cp>\u003cspan class=\"right\">\u003ca href=\"http://www.flickr.com/photos/kqedquest/2516284073/\" title=\"1b. How to make a volcano by kqedquest, on Flickr\">\u003cimg src=\"http://farm3.static.flickr.com/2249/2516284073_b277cb0a87_m.jpg\" width=\"240\" height=\"161\" alt=\"1b. How to make a volcano\">\u003c/a>\u003c/span>Volcanoes are formed by a host of geological processes-- in particular, one called subduction. During subduction, one of the earth's plates moves over another, pushing the underlying plate down toward the hotter parts of the earth. These giant slabs of earth are made of a variety of rocks and minerals, some of which melt before others as they sink toward the hot mantle. The melted rock, called magma, is lighter and more buoyant than the rocks around and above it. The magma makes its way upward through the earth's crust, often explosively, creating a volcano.\u003c/p>\n\u003cp>When subduction stops, the fuel that fires a volcano slowly wanes. Here in Northern California, subduction has been slowing in a northward pattern. In other words, volcanic activity stopped first in the southern stretches near Hollister, then near Oakland, then in Sonoma. The area's volcanic rocks get younger and younger as you move northward, until you reach Mt. Lassen, a still active vent that last erupted in 1917.\u003c/p>\n\u003ch3>The story behind Sibley's special volcano\u003c/h3>\n\u003cp>In its early days, Round Top was just a burbling crater. As it erupted, it filled itself with its own volcanic debris and, in time, lava piling on lava created a peak. With more eruptions, the volcano buried itself under hundreds of feet of lava and volcanic ash. \u003c/p>\n\u003cp>Then, nearby faults began to shift. Slices of the earth's crust moved northward, pushing and bumping things up against each other, creating folds and twists in the landscape. Caught in the action, the land under Round Top began to lean eastward, lifting and tilting until the volcano and all its roots were completely pushed over. The softer rocks that were exposed by this process eroded away, leaving behind a volcanic cauldron filled with its own material, its peak pointing to the east, toward the Sierra Nevada.\u003c/p>\n\u003cp>To help visualize Round Top's story, imagine the East Bay a bit differently than you usually do: it's no longer a series of neighborhoods comprising Berkeley and Oakland and nearby cities. It's one sprawling, continuous geological story. \u003c/p>\n\u003cp>The tale is centered at Round Top, which is situated near the juncture of Skyline and Grizzly Peak boulevards in the Oakland hills. But the story streams out from there, across parts of the East Bay landscape. Each day, thousands of cars pass by one strand of it, a 150-foot-thick lava flow exposed just east of the Caldecott tunnel. Next time you're on that stretch of Highway 24, look up at the road cut. The dark brown diagonal rocks forming the high part of the cliff are made of a hardened volcanic rock called basalt.You're driving by lava that erupted from nearby Round Top ten million years ago.\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003ca href=\"http://www.flickr.com/photos/kqedquest/2516296191/\" title=\"9a. Welded cinder by kqedquest, on Flickr\">\u003cimg src=\"http://farm4.static.flickr.com/3111/2516296191_a714d06802_m.jpg\" width=\"240\" height=\"161\" alt=\"9a. Welded cinder\">\u003c/a>\u003c/span>Southeast of the tunnel, the rocks in Sibley park recount a variety of volcanic events. Outcrops of red and brown rocks record the impact of the steaming lava as it first rolled out onto the cooling surface of the earth. Two rows of broken basalts straddle a more fine-grained rock that was once a fluid lava that moved between the two cooling outer layers. And orange-ish blobs hiding in patches of grass are the result of lava fragments that welded together as they were flying from the volcano, a rare formation, and possibly the only example of it that you can see in California.\u003c/p>\n\u003cp>While all these structures leave us impressed with Round Top's activity in its heyday, what really sets Sibley's volcano apart is that it reveals its inner workings to the public in a way rarely seen. Park visitors get a real geology lesson along with these interesting rock formations. To make matters even more revealing, Kaiser Sand and Gravel quarried the area comprising the park years ago. In doing so, they exposed the heart of the volcano, giving park visitors even more history to gander at. Hike out to the quarries and you'll find a variety of rock types in the remains of the quarry pits: hard basalt that was injected into the volcano, forming lakes inside it, and lighter materials like volcanic ash and mud that have been pushed up from horizontal to vertical.\u003c/p>\n\u003ch3>Geologists love road cuts and quarries\u003c/h3>\n\u003cp>While digging and blasting the ground might pose some hazards to local biology, such acts can also reveal remarkable aspects of the earth that would otherwise remain hidden. \"Geologists love road cuts and quarries,\" says paleobotanist Steve Edwards, who mapped Round Top's history as part of his doctorate work. \"It's like an outdoor classroom, an incomparable display.\" And Sibley, in particular, presents visitors with rare opportunities. \"There is no other volcano in California whose deep interior is similarly exposed. It's a totally unique site,\" he says. \"It's absolutely incredible that we have this.\"\u003c/p>\n\u003ch2>Get Involved\u003c/h2>\n\u003cp>Without the help of dedicated volunteers and docents, the East Bay Regional Park District could not offer the public the variety of services and programs that it does. There are many year-round volunteer and docent opportunities for you, your family, or your school or civic group in the Regional Parks. For information, email us at \u003ca href=\"mailto:Volunteers@EBParks.org\">Volunteers@EBParks.org\u003c/a> or visit \u003ca href=\"http://www.ebparks.org/about/getinvolved/volunteer\">the East Bay Regional Park District's website\u003c/a> for upcoming volunteer opportunities.\u003c/p>\n\u003ch2>Latest Visitor Photos\u003c/h2>\n\u003cp>[ad floatright]\u003c/p>\n\u003cp>Join the \u003ca href=\"http://flickr.com/groups/835115@N22\">Sibley Volcanic Regional Preserve photo group on Flickr\u003c/a> to share your photos of this amazing place.\u003c/p>\n\u003ch2>Additional Links\u003c/h2>\n\u003cul>\n\u003cli>\u003ca href=\"http://www.ebparks.org/parks/sibley\">Sibley Volcanic Regional Preserve\u003c/a>\u003c/li>\n\u003cli>\u003ca href=\"http://vulcan.wr.usgs.gov/Volcanoes/California/framework.html\">California Volcanoes and Volcanics\u003c/a>\u003c/li>\n\u003cli>\u003ca href=\"http://baynature.org/articles/apr-jun-2005/voice-of-the-volcano\">Bay Nature: Voice of the Volcano\u003c/a>\u003c/li>\n\u003c/ul>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp align=\"center\">\u003cem>This Exploration created in collaboration with the \u003c/em>\u003ca href=\"http://www.exploratorium.edu\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/imp/explo_logo_black3.gif\" border=\"0\">\u003c/a>\u003c/p>\n\u003cp>\u003c!-- iframe plugin v.4.3 wordpress.org/plugins/iframe/ -->\u003cbr>\n\u003ciframe src=\"http://www.everytrail.com/guide/sibley-volcanic-regional-preserve-exploration/map?embed=true\" marginheight=\"0\" marginwidth=\"0\" frameborder=\"0\" scrolling=\"no\" width=\"980\" height=\"450\" class=\"iframe-class\">\u003c/iframe>\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003c/span>As sure as the earth moves in Oakland, there's a volcano just off Skyline Boulevard. Not just any volcano, mind you. This one's lying on its side with its guts exposed. You might not recognize it right away, owing to its reclining position and the grassy coat it's adopted. But among the shrubs and grasses at Sibley Volcanic Regional Preserve, you'll find the rocky body and underpinnings of one of the largest of a handful of volcanoes that once dotted our geologic neighborhood. Join us and naturalist Steve Edwards of the East Bay Regional Park District on our latest Bay Area science hike.\u003c/p>\n\u003ch3>Location\u003c/h3>\n\u003cp>6800 Skyline Blvd, Oakland, CA 94611 [\u003ca href=\"http://tinyurl.com/6lj4lr\">Map\u003c/a>]\u003cbr>\nPhone: 888-EBPARKS (888-327-2757), option 3, extension 4554\u003c/p>\n\u003cp>Open between 5 a.m. and 10 p.m. unless otherwise posted or permitted\u003cbr>\n\u003ca href=\"http://www.ebparks.org/parks/sibley\">Download a trail map\u003c/a> and more about the park.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cem>Special thanks to Steve Edwards, Isa Polt-Jones and Rosemary Cameron of the \u003ca href=\"http://www.ebparks.org\">East Bay Regional Parks District\u003c/a> for their participation.\u003c/em>\u003cbr>\n\u003cem>Robin Marks contributed to this Exploration.\u003c/em>\u003c/p>\n\u003ch2>Sibley's Round Top: A Sideways Volcano\u003c/h2>\n\u003ch3>Volcanoes in the East Bay? Really?\u003c/h3>\n\u003cp>\u003cspan class=\"right\">\u003cimg src=\"http://farm3.static.flickr.com/2082/2516290125_6cbb5fd770_m.jpg\" width=\"240\" height=\"161\">\u003c/span>As sure as the earth moves in Berkeley, there's a volcano just off Skyline Boulevard. Not just any volcano, mind you. This one's laying on its side with its guts exposed. You might not recognize it right away, owing to its reclining position and the grassy coat it's adopted. But among the shrubs and grasses at Sibley Regional Volcanic Preserve, you'll find the rocky body and layered underpinnings of one of the largest of a handful of volcanoes that once dotted our geologic neighborhood.\u003c/p>\n\u003cp>Ten million years ago, a vent now called Round Top sprouted in the Earth's crust and regularly spewed thick, gooey lava into its environs. At that time, Round Top stood upright, like a proper volcano, south of present-day San Jose. Over the millennia, the volcano's been ferried northward by the motion of nearby faults, a rugged journey that's changed the appearance of the mountain and the land around it.\u003c/p>\n\u003ch3>A few volcanic basics\u003c/h3>\n\u003cp>\u003cspan class=\"right\">\u003ca href=\"http://www.flickr.com/photos/kqedquest/2516284073/\" title=\"1b. How to make a volcano by kqedquest, on Flickr\">\u003cimg src=\"http://farm3.static.flickr.com/2249/2516284073_b277cb0a87_m.jpg\" width=\"240\" height=\"161\" alt=\"1b. How to make a volcano\">\u003c/a>\u003c/span>Volcanoes are formed by a host of geological processes-- in particular, one called subduction. During subduction, one of the earth's plates moves over another, pushing the underlying plate down toward the hotter parts of the earth. These giant slabs of earth are made of a variety of rocks and minerals, some of which melt before others as they sink toward the hot mantle. The melted rock, called magma, is lighter and more buoyant than the rocks around and above it. The magma makes its way upward through the earth's crust, often explosively, creating a volcano.\u003c/p>\n\u003cp>When subduction stops, the fuel that fires a volcano slowly wanes. Here in Northern California, subduction has been slowing in a northward pattern. In other words, volcanic activity stopped first in the southern stretches near Hollister, then near Oakland, then in Sonoma. The area's volcanic rocks get younger and younger as you move northward, until you reach Mt. Lassen, a still active vent that last erupted in 1917.\u003c/p>\n\u003ch3>The story behind Sibley's special volcano\u003c/h3>\n\u003cp>In its early days, Round Top was just a burbling crater. As it erupted, it filled itself with its own volcanic debris and, in time, lava piling on lava created a peak. With more eruptions, the volcano buried itself under hundreds of feet of lava and volcanic ash. \u003c/p>\n\u003cp>Then, nearby faults began to shift. Slices of the earth's crust moved northward, pushing and bumping things up against each other, creating folds and twists in the landscape. Caught in the action, the land under Round Top began to lean eastward, lifting and tilting until the volcano and all its roots were completely pushed over. The softer rocks that were exposed by this process eroded away, leaving behind a volcanic cauldron filled with its own material, its peak pointing to the east, toward the Sierra Nevada.\u003c/p>\n\u003cp>To help visualize Round Top's story, imagine the East Bay a bit differently than you usually do: it's no longer a series of neighborhoods comprising Berkeley and Oakland and nearby cities. It's one sprawling, continuous geological story. \u003c/p>\n\u003cp>The tale is centered at Round Top, which is situated near the juncture of Skyline and Grizzly Peak boulevards in the Oakland hills. But the story streams out from there, across parts of the East Bay landscape. Each day, thousands of cars pass by one strand of it, a 150-foot-thick lava flow exposed just east of the Caldecott tunnel. Next time you're on that stretch of Highway 24, look up at the road cut. The dark brown diagonal rocks forming the high part of the cliff are made of a hardened volcanic rock called basalt.You're driving by lava that erupted from nearby Round Top ten million years ago.\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003ca href=\"http://www.flickr.com/photos/kqedquest/2516296191/\" title=\"9a. Welded cinder by kqedquest, on Flickr\">\u003cimg src=\"http://farm4.static.flickr.com/3111/2516296191_a714d06802_m.jpg\" width=\"240\" height=\"161\" alt=\"9a. Welded cinder\">\u003c/a>\u003c/span>Southeast of the tunnel, the rocks in Sibley park recount a variety of volcanic events. Outcrops of red and brown rocks record the impact of the steaming lava as it first rolled out onto the cooling surface of the earth. Two rows of broken basalts straddle a more fine-grained rock that was once a fluid lava that moved between the two cooling outer layers. And orange-ish blobs hiding in patches of grass are the result of lava fragments that welded together as they were flying from the volcano, a rare formation, and possibly the only example of it that you can see in California.\u003c/p>\n\u003cp>While all these structures leave us impressed with Round Top's activity in its heyday, what really sets Sibley's volcano apart is that it reveals its inner workings to the public in a way rarely seen. Park visitors get a real geology lesson along with these interesting rock formations. To make matters even more revealing, Kaiser Sand and Gravel quarried the area comprising the park years ago. In doing so, they exposed the heart of the volcano, giving park visitors even more history to gander at. Hike out to the quarries and you'll find a variety of rock types in the remains of the quarry pits: hard basalt that was injected into the volcano, forming lakes inside it, and lighter materials like volcanic ash and mud that have been pushed up from horizontal to vertical.\u003c/p>\n\u003ch3>Geologists love road cuts and quarries\u003c/h3>\n\u003cp>While digging and blasting the ground might pose some hazards to local biology, such acts can also reveal remarkable aspects of the earth that would otherwise remain hidden. \"Geologists love road cuts and quarries,\" says paleobotanist Steve Edwards, who mapped Round Top's history as part of his doctorate work. \"It's like an outdoor classroom, an incomparable display.\" And Sibley, in particular, presents visitors with rare opportunities. \"There is no other volcano in California whose deep interior is similarly exposed. It's a totally unique site,\" he says. \"It's absolutely incredible that we have this.\"\u003c/p>\n\u003ch2>Get Involved\u003c/h2>\n\u003cp>Without the help of dedicated volunteers and docents, the East Bay Regional Park District could not offer the public the variety of services and programs that it does. There are many year-round volunteer and docent opportunities for you, your family, or your school or civic group in the Regional Parks. For information, email us at \u003ca href=\"mailto:Volunteers@EBParks.org\">Volunteers@EBParks.org\u003c/a> or visit \u003ca href=\"http://www.ebparks.org/about/getinvolved/volunteer\">the East Bay Regional Park District's website\u003c/a> for upcoming volunteer opportunities.\u003c/p>\n\u003ch2>Latest Visitor Photos\u003c/h2>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Join the \u003ca href=\"http://flickr.com/groups/835115@N22\">Sibley Volcanic Regional Preserve photo group on Flickr\u003c/a> to share your photos of this amazing place.\u003c/p>\n\u003ch2>Additional Links\u003c/h2>\n\u003cul>\n\u003cli>\u003ca href=\"http://www.ebparks.org/parks/sibley\">Sibley Volcanic Regional Preserve\u003c/a>\u003c/li>\n\u003cli>\u003ca href=\"http://vulcan.wr.usgs.gov/Volcanoes/California/framework.html\">California Volcanoes and Volcanics\u003c/a>\u003c/li>\n\u003cli>\u003ca href=\"http://baynature.org/articles/apr-jun-2005/voice-of-the-volcano\">Bay Nature: Voice of the Volcano\u003c/a>\u003c/li>\n\u003c/ul>\n\n\u003c/div>\u003c/p>",
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"content": "\u003cp>\u003cstrong>Talk about a wild ride.\u003c/strong>\u003c/p>\n\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/louversystem1.jpg\" alt=\"\">\u003c/span>Every year, millions of fish make a strange and harrowing detour through the \u003ca href=\"http://www.publicaffairs.water.ca.gov/swp/future.cfm\">Skinner Fish Facility\u003c/a>, part of the State Water Project's facilities in the Delta.\u003c/p>\n\u003cp>In my last post, I wrote about \u003ca href=\"http://ww2.kqed.org/quest/2008/06/05/where-water-runs-uphill/\">my visit to the Banks Pumping Plant\u003c/a>, whose giant pumps slurp water from the Delta to help quench California's thirst. As the volumes of water are sucked up, both resident and migrating fish come along for the ride. The Skinner Facility, in operation since 1968, was built to protect fish from being killed at the pumps--an effort that sadly is not as successful as one would hope (more on that below).\u003c/p>\n\u003cp>I was amazed to learn there is a whole art and science to fish screens, which range from physical barriers--called \u003cem>positive barriers\u003c/em>--like perforated plates or wire mesh, to \u003cem>behavioral barriers\u003c/em> like sound, light, or other stimuli aimed at keeping fish away. Well-designed screens minimize both \u003cem>entrainment\u003c/em> (fish being pulled into the pump or diversion) and \u003cem>impingement\u003c/em> (fish being trapped or injured against the screen itself due to water velocity).\u003c/p>\n\u003cp>Both physical and behavioral barriers are used at the Skinner Facility. Fish being pulled toward the pumps first encounter a trash rack that diverts many bigger fish, along with floating debris. Next, fish encounter a large, v-shaped array of metal louvers. The louvers create turbulence that functions as a behavioral signal, encouraging the fish to swim away into bypass pipes that function, as our tour guide put it, like \"a big vacuum system.\"\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/holdingtank1.jpg\" alt=\"\">\u003c/span>From the bypass pipes fish travel to another set of louvers and pipes, concentrating them into a smaller volume of water, and then into holding tanks in a nearby warehouse. Giant, suspended cone-shaped buckets are used to periodically sample the fish, which are identified, counted, and measured. Some 90 species turn up in the facility, including \u003ca href=\"http://en.wikipedia.org/wiki/Chinook_salmon\">Chinook salmon\u003c/a>, \u003ca href=\"http://en.wikipedia.org/wiki/Steelhead\">steelhead\u003c/a>, \u003ca href=\"http://en.wikipedia.org/wiki/White_sturgeon\">white sturgeon\u003c/a>, and \u003ca href=\"http://ww2.kqed.org/quest/2007/04/05/little-fish-big-crisis/\">delta smelt\u003c/a>. (I asked our guide if delta smelt really do smell like cucumbers. He confirmed it. In fact, when a school of smelt comes through--an event that has become rare--the warehouse smells \"like a salad.\") When enough fish have been collected, they are loaded into trucks and driven back to the Delta.\u003c/p>\n\u003cp>Here's the rub. Many fish caught in the pull of the pumps are lost to predation before even reaching the screening facility. Then, the facility does not effectively screen fish smaller than about 1.5 inches, meaning that littler, less powerful species and juveniles are still vulnerable to the pumps. For the fish that make it to the holding tanks, the process is such a trauma--with big and little fish squashed together in the tanks, buckets, and trucks--it's no surprise there are casualties; in fact, the delicate delta smelt often do not survive. And even for fish that make it through the entire process and out the other end, there's a final, fatal hurdle: the trunks routinely dump salvaged fish at the same locations, where more predators have learned to cluster for a free lunch.\u003c/p>\n\u003cp>Scientists agree that the loss of fish at the huge state pumps--and other pumps and intake pipes throughout the Delta--is a major contributor to plummeting populations. How much water we use makes a difference: The higher the export rates, the more fish are entrained. There also is broad consensus that more state-of-the-art fish screening facilities are needed. That could come with a hefty price tag. But with our fish disappearing, can we afford \u003cem>not\u003c/em> to invest in their survival?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>37.825718 -121.596422\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cstrong>Talk about a wild ride.\u003c/strong>\u003c/p>\n\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/louversystem1.jpg\" alt=\"\">\u003c/span>Every year, millions of fish make a strange and harrowing detour through the \u003ca href=\"http://www.publicaffairs.water.ca.gov/swp/future.cfm\">Skinner Fish Facility\u003c/a>, part of the State Water Project's facilities in the Delta.\u003c/p>\n\u003cp>In my last post, I wrote about \u003ca href=\"http://ww2.kqed.org/quest/2008/06/05/where-water-runs-uphill/\">my visit to the Banks Pumping Plant\u003c/a>, whose giant pumps slurp water from the Delta to help quench California's thirst. As the volumes of water are sucked up, both resident and migrating fish come along for the ride. The Skinner Facility, in operation since 1968, was built to protect fish from being killed at the pumps--an effort that sadly is not as successful as one would hope (more on that below).\u003c/p>\n\u003cp>I was amazed to learn there is a whole art and science to fish screens, which range from physical barriers--called \u003cem>positive barriers\u003c/em>--like perforated plates or wire mesh, to \u003cem>behavioral barriers\u003c/em> like sound, light, or other stimuli aimed at keeping fish away. Well-designed screens minimize both \u003cem>entrainment\u003c/em> (fish being pulled into the pump or diversion) and \u003cem>impingement\u003c/em> (fish being trapped or injured against the screen itself due to water velocity).\u003c/p>\n\u003cp>Both physical and behavioral barriers are used at the Skinner Facility. Fish being pulled toward the pumps first encounter a trash rack that diverts many bigger fish, along with floating debris. Next, fish encounter a large, v-shaped array of metal louvers. The louvers create turbulence that functions as a behavioral signal, encouraging the fish to swim away into bypass pipes that function, as our tour guide put it, like \"a big vacuum system.\"\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cspan class=\"right\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/07/holdingtank1.jpg\" alt=\"\">\u003c/span>From the bypass pipes fish travel to another set of louvers and pipes, concentrating them into a smaller volume of water, and then into holding tanks in a nearby warehouse. Giant, suspended cone-shaped buckets are used to periodically sample the fish, which are identified, counted, and measured. Some 90 species turn up in the facility, including \u003ca href=\"http://en.wikipedia.org/wiki/Chinook_salmon\">Chinook salmon\u003c/a>, \u003ca href=\"http://en.wikipedia.org/wiki/Steelhead\">steelhead\u003c/a>, \u003ca href=\"http://en.wikipedia.org/wiki/White_sturgeon\">white sturgeon\u003c/a>, and \u003ca href=\"http://ww2.kqed.org/quest/2007/04/05/little-fish-big-crisis/\">delta smelt\u003c/a>. (I asked our guide if delta smelt really do smell like cucumbers. He confirmed it. In fact, when a school of smelt comes through--an event that has become rare--the warehouse smells \"like a salad.\") When enough fish have been collected, they are loaded into trucks and driven back to the Delta.\u003c/p>\n\u003cp>Here's the rub. Many fish caught in the pull of the pumps are lost to predation before even reaching the screening facility. Then, the facility does not effectively screen fish smaller than about 1.5 inches, meaning that littler, less powerful species and juveniles are still vulnerable to the pumps. For the fish that make it to the holding tanks, the process is such a trauma--with big and little fish squashed together in the tanks, buckets, and trucks--it's no surprise there are casualties; in fact, the delicate delta smelt often do not survive. And even for fish that make it through the entire process and out the other end, there's a final, fatal hurdle: the trunks routinely dump salvaged fish at the same locations, where more predators have learned to cluster for a free lunch.\u003c/p>\n\u003cp>Scientists agree that the loss of fish at the huge state pumps--and other pumps and intake pipes throughout the Delta--is a major contributor to plummeting populations. How much water we use makes a difference: The higher the export rates, the more fish are entrained. There also is broad consensus that more state-of-the-art fish screening facilities are needed. That could come with a hefty price tag. But with our fish disappearing, can we afford \u003cem>not\u003c/em> to invest in their survival?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>37.825718 -121.596422\u003c/p>\n\n\u003c/div>\u003c/p>",
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"info": "Possible is hosted by entrepreneur Reid Hoffman and writer Aria Finger. Together in Possible, Hoffman and Finger lead enlightening discussions about building a brighter collective future. The show features interviews with visionary guests like Trevor Noah, Sam Altman and Janette Sadik-Khan. Possible paints an optimistic portrait of the world we can create through science, policy, business, art and our shared humanity. It asks: What if everything goes right for once? How can we get there? Each episode also includes a short fiction story generated by advanced AI GPT-4, serving as a thought-provoking springboard to speculate how humanity could leverage technology for good.",
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"soldout": {
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