The Tibetan Plateau is the
largest high elevation area on the Earth today, and is so elevated and large
that it causes the jet stream to seasonally migrate hundreds of miles- but how
and when did it develop?
Dr. Petr Yakovlev, a geologist at the Montana Bureau of Mines and Geology, kicked off the ISU Geosciences Department Colloquium Series by providing insights into those questions from his PhD work at the University of Michigan. He calculated the crustal mass balance for the region, and determined that the current crustal volume and total convergence requires a thick proto-plateau and redistribution of Indian crust under that plateau. Dr. Yakovlev also spent time in the field in Tibet mapping and dating faults, and there he observed an unusual type of high-elevation compressional deformation that is driven by simple shear and does not produce crustal thickening. Finally, he worked with other scientists studying the Tibetan Plateau to compile a geochemical database for all lavas measured in the region, and found that volcanism with similar evolved-mantle sourcing was widespread across the Plateau beginning around 30 million years ago. He suggests this occurred because the subducted slab of Indian crust broke off into the mantle at that time, 20 million years earlier than previously thought.
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In other Geology Department news,
Professor Sarah Godsey hosted a contest to guess the opening day of Pebble
Creek Ski Area and the winners have been announced! No one correctly guessed
the opening day of December 16th, but four people guessed the 15th
and three people guessed the 17th. Two winners out of this pool were
chosen to split the $50 prize. Congratulations to Dave and Jeff!
And for the data nerds out there,
here are the guesses from this year’s contest compared with the opening dates
from the past five years:
Special thanks to Petr and Sarah
for sharing their figures and data for this story. Writing by Caitlin Rushlow.
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