Large -- Medium The poodle Taun We watches as we pack. |
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Large -- Medium Gwen climbs to the rim of Kilbourne hole, a giant volcanic crater in southern New Mexico, near El Paso. |
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Large -- Medium The crew looks out on the floor of Kilbourne Hole. |
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Large -- Medium The reason we came to Kilbourne Hole is that during this particular volcanic event, the lava, as it upwelled through the lower layers of the Earth, took some of those lower layers with it as the lava rushed to the surface. These blebs of foreign material that get thrown out of the volcano are called xenoliths. We were looking for them. |
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Large -- Medium To find them, we went down to a layer above the lava flows (black basaltic rock) band in the lower layers of volcanic ash (light brown stuff). |
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Large -- Medium We found some! These greenish crystals are composed of olivene and pyroxene, the minerals that make up Earth's mantle (and the mantles of all other rocky planets, too). The mantle makes up over 80% of the Earth by volume. |
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Large -- Medium On the ledge looking for xenoliths -- L to R Gordon Osinski (Oz), Curtis Cooper, Tamara Goldin, Dave Kring, Jani Radebaugh, John Moores, Carl Hergenrother, and Jim Richardson. |
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Large -- Medium A great shot of a mantle xenolith. |
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Large -- Medium Jay Melosh found a motherlode xenolith. |
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Large -- Medium Jani Radebaugh drops acid on the rock to test its composition as Oleg Abramov and Jim Richardson look on. |
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Large -- Medium It fizzed, so Jani interpreted it to be limestone. |
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Large -- Medium Later, John Moores and I found our own motherlode xenolith just peeking out from the ash. They're covered in basalt, since they erupted in lava, so they don't look different until you cut them open. |
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Large -- Medium This xenolith is probably from the lower crust. |
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Large -- Medium We camped right below the rim of Kilbourne Hole on the night of day 1. |