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Tank tracks crossing multiple strands of the fault in one of the complex zones of faulting. |
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The helicopter that flew us to our site. |
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Aerial view of the fault, which cuts across the photo from bottom to top. |
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The fresh fault scarp cutting across a hill. What appears as a roadcut did not exist at all before the earthquake. |
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The fault cuts up a hill. Notice the right-lateral offset of the ridge in the foreground. |
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Close-up of the ridge in the previous shot. |
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A fellow geologist and I, standing on two piercing points of the fault (in this case, an offset terrace riser). Before the earthquake, we would have been standing shoulder-to-shoulder. |
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Another two piercing points (this time, a small stream channel). Again, before the earthquake, we would have been standing shoulder-to-shoulder. |
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Yet another two piercing points (this time, the main stream channel). Once again, before the earthquake, we would have been standing shoulder-to-shoulder. |
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A small vertical scarp formed in the earthquake by the fault. |
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A geologist at work: surveying some fault cracks and offsets. |
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Using a total station to survey offsets. |
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As above, this time it was my turn. Note the fault scarp in the background. |
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The fault cutting across Lavic Lake playa (dry lake bed), creating a "mole track." |
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A fellow geologist stands in the fault crack. |
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That's me in the fault. And I wasn't even as far down as I could go. |
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Another view of the same. Note that the far side of the fault was raised slightly; this was in addition to more than 4 m of right-lateral offset at this site. |
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Me in the fault again. |
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Unexploded ordinance sits next to the fault. Remember, the rupture occurred right in the middle of the bombing range on Twentynine Palms Marine Training Center. |
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One last posed shot before sunset, of geologists at work. |