K/T Boundary Fieldtrip
28 Spetember - 1 October, 2006



For the Fall 2006 fieldtrip, we headed over to New Mexico to check out the K/T boundary deposits. These dposits were created at the end of the Cretaceous period and the start of the Tertiary period. This also marks the end of the age of the dinosaurs due to the large impact that produced the Chicxulub crater (off the coast of Mexico) and the subsequent rise of the age of mammals. This thin clay layer is also enriched in irridium, another clue as to its origin.

The trip was fantastic - some excellent sites that I hadn't seen before, no major mechanical issues and just two slight cases of drunkeness . . . and no, neither one of them were me!


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The Salt River Canyon, our first talk stop
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The Salt River
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Listening to Catherine's talk on spheroidal weathering
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The spheroidal weathering outcrop we were examining
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Betty and Mike at the base of the outcrop
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I loved the erosion patterns here
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Petroglyphs across the road from the outcrop
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Whatever, I had to make sure there was one of me in here somewhere!
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Looking across the Springerville Volcanic Field, the site of my talk
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Jay's cabin at dawn
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Jointing at the La Ventana natural arch stop
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The El Malpais National Park where there has been vocanic activity as recently as 3,000 years ago
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Kat looking over the overlook
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Rory and Mandy
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So now there are 2 pictures of me on the fieldtrip!
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Listening to Eric's talk
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The view from our campsite near Trinidad, CO, on the morning of day 3.
Yes, they're the Rockies.
Yes, that's snow on them.
Yes, it was cold.
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Photo from David O'Brien
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Madrid East, the first place we stopped for the K/T boundary layer
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The light grey layer is the K/T boundary, overlain by a coal deposit and then sandstone
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Everyone up on the outcrop
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Looking up the sandstone to the top of the outcrop
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Colin at our second K/T stop, Longs Canyon
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The K/T boundary at Longs Canyon
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Sliding back down the slope
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Digging out samples at our last K/T stop near Starkville, the only place we could take samples from.