A documentary study of the felt effects of the great California earthquake of 1857
We have collected over 60 hitherto unpublished accounts of the California earthquake of January 9, 1857. We have used them, together with those already known, to estimate felt intensities and prepare an isoseismal map which roughly indicates the level of short-period ground motion experienced during...
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sg-ntu-dr.10356-955952019-12-06T19:17:58Z A documentary study of the felt effects of the great California earthquake of 1857 Sieh, Kerry Agnew, Duncan Carr We have collected over 60 hitherto unpublished accounts of the California earthquake of January 9, 1857. We have used them, together with those already known, to estimate felt intensities and prepare an isoseismal map which roughly indicates the level of short-period ground motion experienced during this earthquake. Modified Mercalli intensities of VI to VII occurred in the modern metropolitan areas of southern California, and VI to VIII in the southern San Joaquin Valley. The intensity along the fault was IX or more. Instances of seiching, fissuring, sandblows, and hydrologic changes were reported from Sacramento to the Colorado River delta. Most reports say that shaking lasted between one and three minutes. At least two large aftershocks occurred within a week of the main event. 2013-03-07T07:39:40Z 2019-12-06T19:17:58Z 2013-03-07T07:39:40Z 2019-12-06T19:17:58Z 1978 1978 Journal Article Agnew, D. C., & Sieh, K. (1978). A documentary study of the felt effects of the great California earthquake of 1857. Bulletin of the Seismological Society of America, 68(6), 1717-1729. 0037-1106 https://hdl.handle.net/10356/95595 http://hdl.handle.net/10220/9354 http://bssa.geoscienceworld.org/content/68/6/1717.abstract en Bulletin of the seismological society of America © 1978 Seismological Society of America |
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We have collected over 60 hitherto unpublished accounts of the California earthquake of January 9, 1857. We have used them, together with those already known, to estimate felt intensities and prepare an isoseismal map which roughly indicates the level of short-period ground motion experienced during this earthquake. Modified Mercalli intensities of VI to VII occurred in the modern metropolitan areas of southern California, and VI to VIII in the southern San Joaquin Valley. The intensity along the fault was IX or more. Instances of seiching, fissuring, sandblows, and hydrologic changes were reported from Sacramento to the Colorado River delta. Most reports say that shaking lasted between one and three minutes. At least two large aftershocks occurred within a week of the main event. |
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Sieh, Kerry Agnew, Duncan Carr |
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Sieh, Kerry Agnew, Duncan Carr A documentary study of the felt effects of the great California earthquake of 1857 |
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Sieh, Kerry Agnew, Duncan Carr |
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Sieh, Kerry |
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A documentary study of the felt effects of the great California earthquake of 1857 |
title_short |
A documentary study of the felt effects of the great California earthquake of 1857 |
title_full |
A documentary study of the felt effects of the great California earthquake of 1857 |
title_fullStr |
A documentary study of the felt effects of the great California earthquake of 1857 |
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A documentary study of the felt effects of the great California earthquake of 1857 |
title_sort |
documentary study of the felt effects of the great california earthquake of 1857 |
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2013 |
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https://hdl.handle.net/10356/95595 http://hdl.handle.net/10220/9354 http://bssa.geoscienceworld.org/content/68/6/1717.abstract |
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