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Ground Water Institute,
University of Memphis
Center for Earthquake
Research and Information
| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
|---|
Memphis, Tennessee, is a location where damaging earthquakes are only moderately likely, but where the consequences of earthquakes, mainly in the New Madrid seismic zone, can be very high (Figure 1). This densely populated urban area is built on a 1-kilometer-thick sequence of sediments deposited in a structural trough known as the Mississippi embayment. Th is thick sequence of sediments significantly affects earthquake ground motions (Bodin et al., 2001; Hashash and Park, 2001).
These urban seismic hazard maps and their derivative products represent the collaborative efforts of the USGS and its partners. A USGS website (http://www.ceri.memphis.edu/usgs/) and Open-File Report 04-1294 (Cramer et al., 2004) document how these seismic hazard maps were generated. The Memphis maps complement the USGS national seismic hazard maps (Frankel et al., 2002), which currently do not include the effects of local geologic structure and variations in soil conditions.
| HAZARD MAPS |
|---|
U.S. Geological Survey
3890 Central Ave.
Memphis, TN
38152-3050
cramer@usgs.gov
(C.H.C.,
J.S.G., E.S.S.)
Ground Water Institute
University of Memphis
Memphis, TN
38152
(B.A.W.)
Center for Earthquake Research and Information
3890 Central
Ave.
Memphis, TN 38152-3050
(K.T.)
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C. H. Cramer, G. J. Rix, and K. Tucker Probabilistic Liquefaction Hazard Maps for Memphis, Tennessee Seismological Research Letters, May 1, 2008; 79(3): 416 - 423. [Full Text] [PDF] |
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