Liquefaction evidence for one or more strong Holocene earthquakes in the Wabash Valley of southern Indiana and Illinois, with a preliminary estimate of magnitude
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Geology topics
Publications and source records attributed to C.A. Munson.
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No abstract available.
Earthquake-induced liquefaction features in Holocene sediments provide evidence of strong prehistoric shaking, magnitude m b 6.2 to 6.7, in the Wabash Valley bordering Indiana and Illinois. The source of the one or more earthquakes responsible was almost certainly in or near the Wabash Valley. The largest event is interpreted to have occurred between 7500 and 1500 years ago on the basis of archeological, pedological, and stratigraphic relations.