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During Spring Break, 2006, Professor Barbara John led 8
students interested in the mechanics of crustal
deformation processes on a tour of the highly extended southern Basin and
Range. The foci of this trip were to investigate the mechanics of faulting
and deformation in mid- to upper crustal regimes,
and to examine the nature of normal fault contacts believed to have formed
and accommodated slip at low-angle orientations (<30 degrees). A three-day
canoe trip down the Colorado River took the group
through the beautiful Topock Gorge, and revealed
impressive geologic relationships in this highly extended region.
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