Artist concept of NASA's New Horizons spacecraft silhouetted with Pluto and its large moon Charon. (NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute/Steve Gribben/Alex Parker)
Seven months after its historic encounter with Pluto, NASA’s New Horizons mission is still dazzling us with discoveries: ancient frozen canyons, chains of icebergs floating in rivers of exotic slush, signs of paleo-oceans, and more.
For a quick flyby mission that lasted mere hours, New Horizons is the gift-giver that keeps on giving as its Pluto data trickles back to Earth.
Icebergs Floating in Nitrogen Slush?
You may have heard of Pluto’s 10,000-foot-high mountain ranges of water ice, possible cryovolcanoes, and nitrogen-ice glaciers pouring through canyons and spilling out into wide flat milky plains. What you may not know is that Pluto has floating islands—yes, islands. Or, maybe more correctly, icebergs, of a sort.
Pluto’s “floating ice islands” in the plains of Sputnik Planum. (NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)
In the smooth white plains of Sputnik Planum, out among the flat expanses of frosty nitrogen and methane, protrude hills of water ice clustered in chains that almost look like flotsam washed up along the banks of a river.
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The water-ice islands, or bergs, range in size from a mile to several miles across. At first glance they appear as hills dotting the flat plain, or possibly the tops of taller formations poking above the frigid flows that surround them.
But the clustering pattern, along with the directional flow of the slushy glacial sheets, suggest that they are large chunks of material that have broken off nearby highlands of water ice and were carried along with the flow.
The clustering in chains may be due to the floating bergs running aground in shallower areas and accumulating—so the impression of riverbank flotsam may be accurate!
In fact, it helps to think of the nitrogen glaciers as rivers and the plains they flood into as seas—seas in a much more literal sense than the “mare” (seas) of Earth’s Moon, which are flat plains of solid basalt.
On Pluto, exotic ices of nitrogen, methane, and ammonia (all of which have been detected in Sputnik Planum) are not rock-solid like their water-ice counterpart, but flow somewhat like glaciers do in Earth’s warmer climate. Glaciers on Earth are even known to carry chunks of rock and transport them from one place to another—although these usually sink to the bottom of the glacier, rock being denser than water ice.
On Pluto, water ice is less dense than the nitrogen glaciers and so would “float” in the slush—not unlike how icebergs float in Earth’s oceans.
Frozen Polar Canyons
Another news flash came in more recently: “frozen” canyons exist in Pluto’s North Pole region—face it, a lot of things are frozen on Pluto. You may think, so what? Isn’t every canyon on Pluto technically frozen? What’s the fuss about?
Pluto’s ancient frozen canyons of its North Polar region. (NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)
The canyons in question are a series of long, parallel furrows, the largest of them gaping 45 miles across, bracketing Pluto’s geographic North Pole. These canyons, unlike many others found elsewhere on Pluto, appear to be quite old, crumbling and degraded with age, and are possibly made of weaker material.
They may be old enough to have formed when Pluto was still tectonically active, when the dwarf planet and its large moon Charon rotated relative to each other and mutually generated a lot of tidal-stress heat.
Today, Pluto and Charon are tidally locked, each keeping the same side aimed at the other—like the faces of a figure-skating couple with gazes locked on one another.
In the tethered grip the pair have on each other today, there is no longer any significant gravitational flexing or stretching between them to generate heat and drive tectonic activity—the figure skaters are not flexing their muscles to perform spins and throws, but simply clasp hands and no longer generate as much body heat.
By studying these polar canyons, scientists may gain insight into conditions in Pluto’s and Charon’s past, when the couple did work up more of a tectonic sweat than today.
Ancient Ocean on Charon?
Finally, turning our attention to Charon (Pluto’s big moon) there appears to be evidence of what may have been an ancient ocean long ago.
The evidence comes in the form of a series of long, deep chasms that give the appearance that Charon’s water ice surface has cracked. One of these “cracks” is 1,100 miles long and up to 4.5 miles deep!
One hypothesis about these epic canyons is that long ago, Charon was warmer, with heat from radioactive decay as well as its initial formation melting at least some of the water ice to form subsurface oceans.
The “cracks” in the icy crust of Pluto’s moon Charon that may be evidence of a past subsurface ocean of liquid water (NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)
As Charon cooled over time, the oceans would have frozen and expanded, pushing the crust outward and forming giant stress fractures—ostensibly the chasms New Horizons captured images of when it flew by last July.
The Adventure Continues
We can enjoy the fruits of New Horizons’ expedition for months to come. Due to the spacecraft’s great distance (presently over 3.2 billion miles from Earth), a limited amount of electrical power, and the fact that it collected many gigabytes of data, it will take upwards of 16 months to transmit it all back to Earth—so the rewards should keep rolling in through the end of this year.
And, there’s a fresh adventure on the horizon, as the tiny nuclear robot coasts toward a 2019 encounter with the Kuiper Belt Object 2014 MU69. If the encounter goes as planned, it will be our first up-close look at a small, icy object in the Kuiper Belt, those vast rings of material that encircle the sun beyond the orbit of Neptune.
Stay tuned…
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"title": "Months After its Pluto Encounter, NASA Spacecraft Still Surprises and Delights",
"headTitle": "Months After its Pluto Encounter, NASA Spacecraft Still Surprises and Delights | KQED",
"content": "\u003cp>Seven months after its historic encounter with Pluto, NASA’s New Horizons mission is still dazzling us with discoveries: ancient frozen canyons, chains of icebergs floating in rivers of exotic slush, signs of paleo-oceans, and more.\u003c/p>\n\u003cp>For a quick flyby mission that lasted mere hours, New Horizons is the gift-giver that keeps on giving as its Pluto data trickles back to Earth.\u003c/p>\n\u003cp>\u003cstrong>Icebergs Floating in Nitrogen Slush?\u003c/strong>\u003c/p>\n\u003cp>You may have heard of Pluto’s 10,000-foot-high mountain ranges of water ice, possible cryovolcanoes, and nitrogen-ice glaciers pouring through canyons and spilling out into wide flat milky plains. What you may not know is that Pluto has \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=408\" target=\"_blank\" rel=\"noopener\">floating islands\u003c/a>—yes, islands. Or, maybe more correctly, icebergs, of a sort.\u003c/p>\n\u003cfigure id=\"attachment_556873\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556873\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-800x480.jpg\" alt=\"Pluto's "floating ice islands" in the plains of Sputnik Planum. \" width=\"800\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-800x480.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-400x240.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-768x461.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-1180x708.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-960x576.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">Pluto’s “floating ice islands” in the plains of Sputnik Planum. \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>In the smooth white plains of\u003ca href=\"http://www.nasa.gov/image-feature/image-of-plutos-vast-icy-plain-informally-called-sputnik-planum\" target=\"_blank\" rel=\"noopener\"> Sputnik Planum\u003c/a>, out among the flat expanses of frosty nitrogen and methane, protrude hills of water ice clustered in chains that almost look like flotsam washed up along the banks of a river.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The water-ice islands, or bergs, range in size from a mile to several miles across. At first glance they appear as hills dotting the flat plain, or possibly the tops of taller formations poking above the frigid flows that surround them.\u003c/p>\n\u003cp>But the clustering pattern, along with the directional flow of the slushy glacial sheets, suggest that they are large chunks of material that have broken off nearby highlands of water ice and were carried along with the flow.\u003c/p>\n\u003cp>The clustering in chains may be due to the floating bergs running aground in shallower areas and accumulating—so the impression of riverbank flotsam may be accurate!\u003c/p>\n\u003cp>In fact, it helps to think of the nitrogen glaciers as rivers and the plains they flood into as seas—seas in a much more literal sense than the “mare” (seas) of Earth’s Moon, which are flat plains of solid basalt.\u003c/p>\n\u003cp>On Pluto, exotic ices of nitrogen, methane, and ammonia (all of which have been detected in Sputnik Planum) are not rock-solid like their water-ice counterpart, but flow somewhat like glaciers do in Earth’s warmer climate. Glaciers on Earth are even known to carry chunks of rock and transport them from one place to another—although these usually sink to the bottom of the glacier, rock being denser than water ice.\u003c/p>\n\u003cp>On Pluto, water ice is less dense than the nitrogen glaciers and so would “float” in the slush—not unlike how icebergs float in Earth’s oceans.\u003c/p>\n\u003cp>\u003cstrong>Frozen Polar Canyons\u003c/strong>\u003c/p>\n\u003cp>Another news flash came in more recently: “frozen” canyons exist in Pluto’s North Pole region—face it, a lot of things are frozen on Pluto. You may think, so what? Isn’t every canyon on Pluto technically frozen? What’s the fuss about?\u003c/p>\n\u003cfigure id=\"attachment_556874\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556874\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-800x986.jpg\" alt=\"Pluto's ancient frozen canyons of its North Polar region. \" width=\"800\" height=\"986\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-800x986.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-400x493.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-768x947.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-1180x1454.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-960x1183.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">Pluto’s ancient frozen canyons of its North Polar region. \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=412\" target=\"_blank\" rel=\"noopener\">canyons in question\u003c/a> are a series of long, parallel furrows, the largest of them gaping 45 miles across, bracketing Pluto’s geographic North Pole. These canyons, unlike many others found elsewhere on Pluto, appear to be quite old, crumbling and degraded with age, and are possibly made of weaker material.\u003c/p>\n\u003cp>They may be old enough to have formed when Pluto was still tectonically active, when the dwarf planet and its large moon Charon rotated relative to each other and mutually generated a lot of tidal-stress heat.\u003c/p>\n\u003cp>Today, Pluto and Charon are tidally locked, each keeping the same side aimed at the other—like the faces of a figure-skating couple with gazes locked on one another.\u003c/p>\n\u003cp>In the tethered grip the pair have on each other today, there is no longer any significant gravitational flexing or stretching between them to generate heat and drive tectonic activity—the figure skaters are not flexing their muscles to perform spins and throws, but simply clasp hands and no longer generate as much body heat.\u003c/p>\n\u003cp>By studying these polar canyons, scientists may gain insight into conditions in Pluto’s and Charon’s past, when the couple did work up more of a tectonic sweat than today.\u003c/p>\n\u003cp>\u003cstrong>Ancient Ocean on Charon?\u003c/strong>\u003c/p>\n\u003cp>Finally, turning our attention to Charon (Pluto’s big moon) there appears to be evidence of what may have been an \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=411\" target=\"_blank\" rel=\"noopener\">ancient ocean\u003c/a> long ago.\u003c/p>\n\u003cp>The evidence comes in the form of a series of long, deep chasms that give the appearance that Charon’s water ice surface has cracked. One of these “cracks” is 1,100 miles long and up to 4.5 miles deep!\u003c/p>\n\u003cp>One hypothesis about these epic canyons is that long ago, Charon was warmer, with heat from radioactive decay as well as its initial formation melting at least some of the water ice to form subsurface oceans.\u003c/p>\n\u003cfigure id=\"attachment_556875\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556875\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-800x433.jpg\" alt=\"The "cracks" in the icy crust of Pluto's moon Charon that may be evidence of a past subsurface ocean of liquid water\" width=\"800\" height=\"433\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-800x433.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-400x217.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-768x416.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-1180x639.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-960x520.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">The “cracks” in the icy crust of Pluto’s moon Charon that may be evidence of a past subsurface ocean of liquid water \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>As Charon cooled over time, the oceans would have frozen and expanded, pushing the crust outward and forming giant stress fractures—ostensibly the chasms New Horizons captured images of when it flew by last July.\u003c/p>\n\u003cp>\u003cstrong>The Adventure Continues\u003c/strong>\u003c/p>\n\u003cp>We can enjoy the fruits of New Horizons’ expedition for months to come. Due to the spacecraft’s great distance (\u003ca href=\"http://pluto.jhuapl.edu/Mission/Where-is-New-Horizons/index.php\" target=\"_blank\" rel=\"noopener\">presently\u003c/a> over 3.2 billion miles from Earth), a limited amount of electrical power, and the fact that it collected many gigabytes of data, it will take upwards of \u003ca href=\"http://gizmodo.com/why-itll-take-new-horizons-16-months-to-send-us-this-we-1717769317\" target=\"_blank\" rel=\"noopener\">16 months to transmit\u003c/a> it all back to Earth—so the rewards should keep rolling in through the end of this year.\u003c/p>\n\u003cp>And, there’s a fresh adventure on the horizon, as the tiny nuclear robot coasts toward a 2019 encounter with the Kuiper Belt Object 2014 MU69. If the encounter goes as planned, it will be our first up-close look at a small, icy object in the Kuiper Belt, those vast rings of material that encircle the sun beyond the orbit of Neptune.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Stay tuned…\u003c/p>\n\n",
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"excerpt": "Seven months after its historic encounter with Pluto, NASA's New Horizons mission is still dazzling us with discoveries: ancient frozen canyons, chains of icebergs floating in rivers of exotic slush, signs of paleo-oceans, and more. ",
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"bio": "\u003cstrong>Benjamin Burress\u003c/strong> has been a staff astronomer at Chabot Space & Science Center since July 1999. He graduated from Sonoma State University in 1985 with a bachelor’s degree in physics (and minor in astronomy), after which he signed on for a two-year stint in the Peace Corps, where he taught physics and mathematics in the African nation of Cameroon. From 1989-96 he served on the crew of NASA’s Kuiper Airborne Observatory at Ames Research Center in Mountain View, CA. From 1996-99, he was Head Observer at the Naval Prototype Optical Interferometer program at Lowell Observatory in Flagstaff, AZ.\r\n\r\nRead his \u003ca href=\"http://science.kqed.org/quest/author/ben-burress/\">previous contributions\u003c/a> to \u003ca href=\"http://science.kqed.org/quest/\">QUEST\u003c/a>, a project dedicated to exploring the Science of Sustainability.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>Seven months after its historic encounter with Pluto, NASA’s New Horizons mission is still dazzling us with discoveries: ancient frozen canyons, chains of icebergs floating in rivers of exotic slush, signs of paleo-oceans, and more.\u003c/p>\n\u003cp>For a quick flyby mission that lasted mere hours, New Horizons is the gift-giver that keeps on giving as its Pluto data trickles back to Earth.\u003c/p>\n\u003cp>\u003cstrong>Icebergs Floating in Nitrogen Slush?\u003c/strong>\u003c/p>\n\u003cp>You may have heard of Pluto’s 10,000-foot-high mountain ranges of water ice, possible cryovolcanoes, and nitrogen-ice glaciers pouring through canyons and spilling out into wide flat milky plains. What you may not know is that Pluto has \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=408\" target=\"_blank\" rel=\"noopener\">floating islands\u003c/a>—yes, islands. Or, maybe more correctly, icebergs, of a sort.\u003c/p>\n\u003cfigure id=\"attachment_556873\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556873\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-800x480.jpg\" alt=\"Pluto's "floating ice islands" in the plains of Sputnik Planum. \" width=\"800\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-800x480.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-400x240.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-768x461.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-1180x708.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16-960x576.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_PlutosFloatingHills-Context-lables_V3-sml-02-04-16.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">Pluto’s “floating ice islands” in the plains of Sputnik Planum. \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>In the smooth white plains of\u003ca href=\"http://www.nasa.gov/image-feature/image-of-plutos-vast-icy-plain-informally-called-sputnik-planum\" target=\"_blank\" rel=\"noopener\"> Sputnik Planum\u003c/a>, out among the flat expanses of frosty nitrogen and methane, protrude hills of water ice clustered in chains that almost look like flotsam washed up along the banks of a river.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The water-ice islands, or bergs, range in size from a mile to several miles across. At first glance they appear as hills dotting the flat plain, or possibly the tops of taller formations poking above the frigid flows that surround them.\u003c/p>\n\u003cp>But the clustering pattern, along with the directional flow of the slushy glacial sheets, suggest that they are large chunks of material that have broken off nearby highlands of water ice and were carried along with the flow.\u003c/p>\n\u003cp>The clustering in chains may be due to the floating bergs running aground in shallower areas and accumulating—so the impression of riverbank flotsam may be accurate!\u003c/p>\n\u003cp>In fact, it helps to think of the nitrogen glaciers as rivers and the plains they flood into as seas—seas in a much more literal sense than the “mare” (seas) of Earth’s Moon, which are flat plains of solid basalt.\u003c/p>\n\u003cp>On Pluto, exotic ices of nitrogen, methane, and ammonia (all of which have been detected in Sputnik Planum) are not rock-solid like their water-ice counterpart, but flow somewhat like glaciers do in Earth’s warmer climate. Glaciers on Earth are even known to carry chunks of rock and transport them from one place to another—although these usually sink to the bottom of the glacier, rock being denser than water ice.\u003c/p>\n\u003cp>On Pluto, water ice is less dense than the nitrogen glaciers and so would “float” in the slush—not unlike how icebergs float in Earth’s oceans.\u003c/p>\n\u003cp>\u003cstrong>Frozen Polar Canyons\u003c/strong>\u003c/p>\n\u003cp>Another news flash came in more recently: “frozen” canyons exist in Pluto’s North Pole region—face it, a lot of things are frozen on Pluto. You may think, so what? Isn’t every canyon on Pluto technically frozen? What’s the fuss about?\u003c/p>\n\u003cfigure id=\"attachment_556874\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556874\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-800x986.jpg\" alt=\"Pluto's ancient frozen canyons of its North Polar region. \" width=\"800\" height=\"986\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-800x986.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-400x493.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-768x947.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-1180x1454.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy-960x1183.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_NorthPoleRotatedContrastUnannotated_CLEAN-copy.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">Pluto’s ancient frozen canyons of its North Polar region. \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=412\" target=\"_blank\" rel=\"noopener\">canyons in question\u003c/a> are a series of long, parallel furrows, the largest of them gaping 45 miles across, bracketing Pluto’s geographic North Pole. These canyons, unlike many others found elsewhere on Pluto, appear to be quite old, crumbling and degraded with age, and are possibly made of weaker material.\u003c/p>\n\u003cp>They may be old enough to have formed when Pluto was still tectonically active, when the dwarf planet and its large moon Charon rotated relative to each other and mutually generated a lot of tidal-stress heat.\u003c/p>\n\u003cp>Today, Pluto and Charon are tidally locked, each keeping the same side aimed at the other—like the faces of a figure-skating couple with gazes locked on one another.\u003c/p>\n\u003cp>In the tethered grip the pair have on each other today, there is no longer any significant gravitational flexing or stretching between them to generate heat and drive tectonic activity—the figure skaters are not flexing their muscles to perform spins and throws, but simply clasp hands and no longer generate as much body heat.\u003c/p>\n\u003cp>By studying these polar canyons, scientists may gain insight into conditions in Pluto’s and Charon’s past, when the couple did work up more of a tectonic sweat than today.\u003c/p>\n\u003cp>\u003cstrong>Ancient Ocean on Charon?\u003c/strong>\u003c/p>\n\u003cp>Finally, turning our attention to Charon (Pluto’s big moon) there appears to be evidence of what may have been an \u003ca href=\"http://pluto.jhuapl.edu/Multimedia/Science-Photos/image.php?page=1&gallery_id=2&image_id=411\" target=\"_blank\" rel=\"noopener\">ancient ocean\u003c/a> long ago.\u003c/p>\n\u003cp>The evidence comes in the form of a series of long, deep chasms that give the appearance that Charon’s water ice surface has cracked. One of these “cracks” is 1,100 miles long and up to 4.5 miles deep!\u003c/p>\n\u003cp>One hypothesis about these epic canyons is that long ago, Charon was warmer, with heat from radioactive decay as well as its initial formation melting at least some of the water ice to form subsurface oceans.\u003c/p>\n\u003cfigure id=\"attachment_556875\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-556875\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-800x433.jpg\" alt=\"The "cracks" in the icy crust of Pluto's moon Charon that may be evidence of a past subsurface ocean of liquid water\" width=\"800\" height=\"433\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-800x433.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-400x217.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-768x416.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-1180x639.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded-960x520.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2016/03/00_Charon_SerenityChasma_Context_02182016_Melded.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">The “cracks” in the icy crust of Pluto’s moon Charon that may be evidence of a past subsurface ocean of liquid water \u003ccite>(NASA/Johns Hopkins University Applied Physics Laboratory/Southwest Research Institute)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>As Charon cooled over time, the oceans would have frozen and expanded, pushing the crust outward and forming giant stress fractures—ostensibly the chasms New Horizons captured images of when it flew by last July.\u003c/p>\n\u003cp>\u003cstrong>The Adventure Continues\u003c/strong>\u003c/p>\n\u003cp>We can enjoy the fruits of New Horizons’ expedition for months to come. Due to the spacecraft’s great distance (\u003ca href=\"http://pluto.jhuapl.edu/Mission/Where-is-New-Horizons/index.php\" target=\"_blank\" rel=\"noopener\">presently\u003c/a> over 3.2 billion miles from Earth), a limited amount of electrical power, and the fact that it collected many gigabytes of data, it will take upwards of \u003ca href=\"http://gizmodo.com/why-itll-take-new-horizons-16-months-to-send-us-this-we-1717769317\" target=\"_blank\" rel=\"noopener\">16 months to transmit\u003c/a> it all back to Earth—so the rewards should keep rolling in through the end of this year.\u003c/p>\n\u003cp>And, there’s a fresh adventure on the horizon, as the tiny nuclear robot coasts toward a 2019 encounter with the Kuiper Belt Object 2014 MU69. If the encounter goes as planned, it will be our first up-close look at a small, icy object in the Kuiper Belt, those vast rings of material that encircle the sun beyond the orbit of Neptune.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Stay tuned…\u003c/p>\n\n\u003c/div>\u003c/p>",
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"soldout": {
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