Geological Society of America Bulletin · 1963 · 11 citations · 0 references
VolcanologyEngineeringSedimentary GeologyEarth ScienceRegional GeologyGsa Bulletin 1963Geological DataRegional TectonicsEastern MexicoGeological EngineeringMarine GeologyGeographyGeologyGsa BulletinTectonicsStructural GeologyExploration GeologyEconomic GeologyEarth SciencesGeochemistryPetrology
Research Article| February 01, 1963 Sedimentary Volcanism in Eastern Mexico and Northern Colombia WILLIAM E HUMPHREY WILLIAM E HUMPHREY American International Oil Company, New York, N. Y Search for other works by this author on: GSW Google Scholar Author and Article Information WILLIAM E HUMPHREY American International Oil Company, New York, N. Y Publisher: Geological Society of America Received: 11 Aug 1962 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1963, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1963) 74 (2): 125–128. https://doi.org/10.1130/0016-7606(1963)74[125:SVIEMA]2.0.CO;2 Article history Received: 11 Aug 1962 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation WILLIAM E HUMPHREY; Sedimentary Volcanism in Eastern Mexico and Northern Colombia. GSA Bulletin 1963;; 74 (2): 125–128. doi: https://doi.org/10.1130/0016-7606(1963)74[125:SVIEMA]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 SocietyGSA Bulletin Search Advanced Search Abstract The active El Cocuite mud volcano in Eastern Mexico and the more quiescent El Totumo mud volcano in Northern Colombia are briefly described. The more volatile behavior of the El Cocuite vent may be attributed to the lower viscosity of its mud, itself a function of the more youthful age and lesser lithification of its source formation. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.