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Invitation to Field Review of Hebgen Lake Paleoseismic Sites |
Last July, researchers from the US Geological
Survey (Denver, Bozeman, and Menlo Park), Lawrence Livermore
National Laboratory, and Montana State University (the Hebgen
Lake Paleoseismology Working Group) jointly conducted paleoseismic
investigations at three sites on the Hebgen fault and Red Canyon
fault in southwest Montana. These subparallel en echelon faults
were the primary structures that ruptured during the 1959
Hebgen Lake earthquake. Even though the Hebgen Lake earthquake
was one of the largest earthquakes in the intermountain west,
the earlier history of these faults is poorly understood. These
investigations, which use classical paleseismology and cosmogenic
isotope dating of alluvial surfaces and a bedrock exposure, were
designed to evaluate the timing of prehistoric events and determine
whether the Hebgen and Red Canyon faults ruptured synchronously
prior to 1959. The northernmost trench site is at Cabin Creek
at the north end of the Hebgen fault. This trench has now been
backfilled but the scarp, terraces, trench logs, and dating results
with will provide the focus for discussion. At the Section 31
site near the middle of the Hebgen fault two open trenches across
the main fault and graben that expose multiple events will be
on view. Immediately south of these trenches is a faulted limestone
exposure that has been the location of sampling and Cl 36 analysis
used for interpretation of earthquake recurrence. The final stop
is southeast of Grayling Creek, near the southeast end of the
Red Canyon fault. Here, one trench across a major graben exposes
the 1959 event and prior deformation. Directions to Cabin Creek from Big Sky,
MT: Take Highway 191 south until a junction with Highway 287.
Turn right towards Hebgen Lake on 287 for ~12 miles until you
see a sign (on the right) for Cabin Creek. |
Phone 213/740-5843 Fax 213/740-0011 e-mail: SCECinfo@usc.edu |