Cordilleran Section - 101st Annual Meeting (April 29–May 1, 2005)

Paper No. 18
Presentation Time: 9:00 AM-5:00 PM

TEPHROCHRONOLOGY OF THE NORTHERN KIT FOX HILLS, DEATH VALLEY, CALIFORNIA


EBBS, Veva Marie, PO Box 6850, Fullerton, 92834, LIDDICOAT, Joseph C., Environmental Science, Barnard College, Columbia Univ, 3009 Broadway, New York, NY 10027-6598, SARNA-WOJCICKI, Andrei M., U. S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025 and KNOTT, Jeffrey R., Department of Geological Sciences, California State Univ, Fullerton, P.O. Box 6850, Fullerton, CA 92834, vevaebbs@hotmail.com

The northern Kit Fox Hills in central-east Death Valley are a pressure ridge adjacent Northern Death Valley fault zone (NDVFZ). To determine the age of the uplifted sediments, I mapped, measured a stratigraphic section and collected samples for tephrochronologic and paleomagnetic analysis. The paleomagnetic data and similarity coefficients (SC) indicate tephra sample VME-KFH-03 correlates with 1.9-1.5 Ma middle Glass Mountain tuffs (SC = 0.9795), and VME-KFH-04 with 0.8-1.2 Ma Upper Glass Mountain ash beds (SC = 0.9902). The overlying VME-KFH-07 correlates with either the Bishop Ash Bed (~0.77 Ma) or a Mesquite Spring tuff (3.1 – 3.3 Ma). Paleomagnetics show the section to be dominantly reverse polarity beginning directly below VME-KFH-07. A normal polarity section is found between VME-KFH-03 and 04. One interpretation is that VME-KFH-07 is the Bishop Ash Bed with the underlying ash beds Upper Glass Mountain and the normal polarity section the Jaramillo subchron. Alternatively, VME-KFH-07 is interpretable as a Mesquite Spring tuff and the underlying ash beds previously undescribed beds with Glass Mountain affinity.