triangular facet

Penrose participants at Mammoth Mountain.

Penrose Conference: Kinematics and Geodynamics of Intraplate Dextral Shear in Eastern California and Western Nevada

April 21-26, 2005: Mammoth Mountain Inn, Mammoth Lakes, California

Conveners
Jeffrey Lee Dept. of Geological Sciences, Central Washington Univ., Ellensburg, WA 98926, (509) 963-2801, email: jeff@geology.cwu.edu
Daniel Stockli Geology Dept., Univ. of Kansas, Lawrence, KS 66045, (785) 864-4995, email: stockli@ku.edu
Christopher Henry Nevada Bureau of Mines and Geology, Univ. of Nevada, Reno, NV, (775) 784-6691, email: chenry@unr.edu
Timothy Dixon RSMAS-MGG, Miami Univ., Miami, FL 33149, (305) 361-4660, email: tdixon@rsmas.miami.edu



Penrose Objectives and Description

Schedule and Keynote Abstracts




triangular facet

View of normal fault scarp and triangular facet along the Queen Valley fault. Vertical surface offset across the scarp is ~6.1 m.



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