Research Article| July 01, 2002 Historical Constraints on Previous Seismic Activity and Morphologic Changes near the Source Zone of the 1819 Rann of Kachchh Earthquake: Further Light on the Penultimate Event C. P. Rajendran; C. P. Rajendran Centre for Earth Science Studies P.B. No. 7250 Akkulam Trivandrum 695031 India cp_r@vsnl.com Search for other works by this author on: GSW Google Scholar Kusala Rajendran Kusala Rajendran Centre for Earth Science Studies P.B. No. 7250 Akkulam Trivandrum 695031 India cp_r@vsnl.com Search for other works by this author on: GSW Google Scholar Author and Article Information C. P. Rajendran Centre for Earth Science Studies P.B. No. 7250 Akkulam Trivandrum 695031 India cp_r@vsnl.com Kusala Rajendran Centre for Earth Science Studies P.B. No. 7250 Akkulam Trivandrum 695031 India cp_r@vsnl.com Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2002 by the Seismological Society of America Seismological Research Letters (2002) 73 (4): 470–479. https://doi.org/10.1785/gssrl.73.4.470 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation C. P. Rajendran, Kusala Rajendran; Historical Constraints on Previous Seismic Activity and Morphologic Changes near the Source Zone of the 1819 Rann of Kachchh Earthquake: Further Light on the Penultimate Event. Seismological Research Letters 2002;; 73 (4): 470–479. doi: https://doi.org/10.1785/gssrl.73.4.470 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search The Kachchh (also spelled Kutch and Cutch) province in the northwestern part of India continues to be remarkably active seismically, the 2001 Bhuj (Mw 7.7) earthquake being the most recent example of the region's seismogenic potential (Figure 1). Among past events, the 1819 earthquake (M > 7.5) is well known and is quoted in the early geologic literature for the dramatic coseismic topographic changes associated with it, including the formation of the elevated tract of land called the Allah Bund (Lyell, 1857). Occurrence of two large earthquakes during a short span of 180... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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