HR: 14:55h
AN: S53C-06 [Abstracts]
TI: Geophysical and Geological Evidence of Neotectonic Deformation Along the Hovey Lake Fault, Lower Wabash
Valley Fault System, Central United States
AU: * Woolery, E W
EM: woolery@uky.edu
AF: University of Kentucky, Dept. of Geological Sciences
101 Slone Building, Lexington, KY 40506
United States
AU: Rutledge, F A
EM: frutledg@vt.edu
AF: Virginia Polytechnic Institute, 19 Patton Hall, Blacksburg, VA 24060
United States
AU: Wang, Z
EM: zmwang@uky.edu
AF: University of Kentucky, Kentucky Geological Survey
228 MMRB, Lexington, KY 40506
United States
AB:
High-resolution seismic (shear-wave) reflection profiles were collected over a segment of the Hovey Lake fault, a known
Paleozoic fault within a system of faults in the southernmost Wabash River valley of the central United States. Although the
system of faults, called the Wabash Valley fault system, lie in an area of recognized prehistoric and contemporary
seismicity, their seismogenic potential remain poorly defined, however. Consequently, the objectives of this study were to
assess the Hovey Lake fault, one of the more prominent fault strands in the system, for neotectonic reactivation, and if
present, collect sediment samples for dateable material from the disrupted horizons to provide an age constraint for the
movement. The resultant stacked profiles show high-angle deformation extending above the Paleozoic bedrock, and into Upper
Quaternary sediment. Time displacement calculations from the data show approximately 10.5 m of offset on the top-of-bedrock
horizon, and 2 m of inverted displacement along the earliest-arriving Quaternary soil reflector at a depth of 5 m.
Preliminary correlative coring found organic material in a disrupted soil horizon located 7.7 m below ground surface.
Subsequent carbon-14 testing of the deeper horizon allows us to place a maximum age constraint at this site of approximately
37,000 YBP.
DE: 7230 Seismicity and seismotectonics
DE: 8010 Fractures and faults
SC: Seismology [S]
MN: 2004 AGU Fall Meeting