Research Article| May 01, 2002 Shelf record of climatic changes in flood magnitude and frequency, north-coastal California Christopher K. Sommerfield; Christopher K. Sommerfield 1University of Delaware, College of Marine Studies, Lewes, Delaware 19958, USA Search for other works by this author on: GSW Google Scholar David E. Drake; David E. Drake 2Drake Marine Consulting, 1711 Quail Hollow Road, Ben Lomond, California 95005, USA Search for other works by this author on: GSW Google Scholar Robert A. Wheatcroft Robert A. Wheatcroft 3Oregon State University, College of Oceanic and Atmospheric Sciences, Corvallis, Oregon 97331, USA Search for other works by this author on: GSW Google Scholar Geology (2002) 30 (5): 395–398. https://doi.org/10.1130/0091-7613(2002)030<0395:SROCCI>2.0.CO;2 Article history received: 28 Aug 2001 rev-recd: 20 Dec 2001 accepted: 20 Dec 2001 first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Christopher K. Sommerfield, David E. Drake, Robert A. Wheatcroft; Shelf record of climatic changes in flood magnitude and frequency, north-coastal California. Geology 2002;; 30 (5): 395–398. doi: https://doi.org/10.1130/0091-7613(2002)030<0395:SROCCI>2.0.CO;2 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 SocietyGeology Search Advanced Search Abstract Continental-shelf deposits off the Eel River, north-coastal California, document a recent increase in the magnitude and frequency of major hydrologic floods (≥10 yr recurrence interval). The shelf record reveals a sudden, three-fold increase in sedimentation rate ca. 1954 and a concomitant increase in the frequency of preserved flood beds. Comparison of sedimentary and river-discharge records reveals that major floods after ca. 1950 had a more pronounced effect on coastal sediment delivery and accumulation offshore than previous recorded events of similar magnitude, and that stratigraphic preservation of flood events is highly dependent on flood frequency and net sedimentation rate. We contend that this change in marine sedimentation is a response to documented climatic phenomena that have increased the frequency of major floods throughout the western United States during the past half century, together with intrabasinal impacts of extreme floods in 1955 and 1964. Anthropogenic increase in watershed-sediment production is a probable secondary factor. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.