CaltechAUTHORS
  A Caltech Library Service

Mudflow of 1941 at Wrightwood, southern California

Sharp, Robert P. and Nobles, Laurence H. (1953) Mudflow of 1941 at Wrightwood, southern California. Geological Society of America Bulletin, 64 (5). pp. 547-560. ISSN 0016-7606. doi:10.1130/0016-7606(1953)64[547:MOAWSC]2.0.CO;2. https://resolver.caltech.edu/CaltechAUTHORS:20140806-150716817

Full text is not posted in this repository. Consult Related URLs below.

Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20140806-150716817

Abstract

During early May of 1941 the southern California mountain resort of Wrightwood was partly inundated by surging flows of muddy debris which occurred daily for more than a week. The immediate cause of flowage was rapid melting of deep winter snow. Intense shattering and rapid weathering of the bedrock (Pelona schist) within the San Andreas rift zone at this location contributed materially to preparing debris for flowage. Field studies, eyewitness accounts, and movie films provide the following information. Debris was transported 15 miles by the mudflow, and on a gradient as low as 75 feet per mile at the outer extremity. The flow advanced in successive waves or surges of “slimy gray cement-like” mud containing abundant stones. Velocities of the surge fronts ranged from a few to nearly 15 feet per second and averaged close to 10 feet per second during the more fluid phases. The fronts of the more fluid surges slithered and splashed along about like a rapidly advancing tongue of water. No breaker-like motion was evident, although the top of the front tended to shoot ahead of the base. In more viscous surges a bouldery embankment developed at the front and was shoved along by the material following behind. One sample of the fluid debris had a density of 2.4, indicating a water content of 25–30 per cent by weight. Calculated viscosities range from 2 × 10^3 to 6 × 10^3 poises. An average sorting coefficient of 3.94 indicates poor sorting, although somewhat better than in many glacial tills which the flow deposits strongly resemble. Earlier mudflows have occurred here, and others will undoubtedly take place in the future.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1130/0016-7606(1953)64[547:MOAWSC]2.0.CO;2DOIArticle
http://bulletin.geoscienceworld.org/content/64/5/547PublisherArticle
Additional Information:Copyright © 1953, The Geological Society of America, Inc. Received July 7, 1952.
Issue or Number:5
DOI:10.1130/0016-7606(1953)64[547:MOAWSC]2.0.CO;2
Record Number:CaltechAUTHORS:20140806-150716817
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140806-150716817
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48130
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:06 Aug 2014 22:34
Last Modified:10 Nov 2021 18:03

Repository Staff Only: item control page