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Major earthquakes recorded by Speleothems in Midwestern U.S. caves

Bulletin of the Seismological Society of America

By:
, , , , , and
DOI: 10.1785/0120080261

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Abstract

Historic earthquakes generated by the New Madrid seismic zone represent some of the largest recorded in the United States, yet prehistoric events are recognized only through deformation in late-Wisconsin to Holocene-age, near surface sediments (liquefaction, monoclinal folding, and changes in river meanders). In this article, we show that speleothems in caves of southwestern Illinois and southeastern Missouri may constitute a previously unrecognized recorder of large earthquakes in the U.S. midcontinent region. The timing of the initiation and regrowth of stalagmites in southwestern Illinois and southeastern Missouri caves is consistent with the historic and prehistoric record of several known seismic events in the U.S. midcontinent region. We conclude that dating the initiation of original stalagmite growth and later postearthquake rejuvenation constitutes a new paleoseismic method that has the potential for being applied to any region around the world in the vicinity of major seismic zones where caves exist. Use of this technique could expand the geographical distribution of paleoseimic data, document prehistoric earthquakes, and help improve interpretations of paleoearthquakes.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Major earthquakes recorded by Speleothems in Midwestern U.S. caves
Series title:
Bulletin of the Seismological Society of America
DOI:
10.1785/0120080261
Volume
99
Issue:
4
Year Published:
2009
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Bulletin of the Seismological Society of America
First page:
2147
Last page:
2154
Number of Pages:
8