1985
DOI: 10.3133/ofr85457
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Estimation of earthquake effects associated with large earthquakes in the New Madrid seismic zone

Abstract: Estimates have been made of the effects of a great earthquake (M = 8.6, I = XI), a large earthquake (M = 7.6, I = X), and a moderate earthquake (M =6.7, I Q = ix) hypothesized to occur anywhere in the New Madrid seismic zone. The estimates are based on the distributions of observed intensities associated with the earthquakes of 1811-12, 1843 and 1895, although the effects of other historical shocks are also considered. The resulting composite type intensity maps for each magnitude are believed to represent the… Show more

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Cited by 9 publications
(6 citation statements)
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“…Comprehensive ground-water flow models can assess water-use management decisions only by 7 BENEFITS OF GEOLOGIC MAPPING incorporating three-dimensional geologic models, accurate hydrologic and hydrogeologic parameters, and measurements of ground-water elevations.…”
Section: Environmental Benefitsmentioning
confidence: 99%
“…Comprehensive ground-water flow models can assess water-use management decisions only by 7 BENEFITS OF GEOLOGIC MAPPING incorporating three-dimensional geologic models, accurate hydrologic and hydrogeologic parameters, and measurements of ground-water elevations.…”
Section: Environmental Benefitsmentioning
confidence: 99%
“…Recent M3 findings call this assumption into question (Sibol and others, 1987;Bollinger and others, 1991;Hanks and Johnston, 1992). The isoseismals cannot be tested against an actual earthquake of about MS 7.6 because the Central United States has had no historical shocks between about M § 6.8 and 8.4 (Hopper, 1985;Johnston, in press).…”
Section: Hypothetical Isoseismalsmentioning
confidence: 99%
“…The studies related to the seismicity of the New Madrid region have always referred to the 1811 and 1812 New Madrid earthquakes as the largest earthquakes known to have occurred in the Mississippi Valley. A general historical seismicity map of the New Madrid seismic zone and surrounding areas is provided in Figure 3, as adopted from Hopper [5].…”
Section: Seismicity Of the Regionmentioning
confidence: 99%