Chattermark trails as paleoenvironmental indicators

Abstract

Research Article| July 01, 1980 Chattermark trails as paleoenvironmental indicators Peter A. Bull; Peter A. Bull 1Christ Church, Oxford, OX1 1DP, England Search for other works by this author on: GSW Google Scholar Stephen J. Culver; Stephen J. Culver 2Department of Paleobiology, Smithsonian Institution, Washington, D.C. 20560 Search for other works by this author on: GSW Google Scholar Rita Gardner Rita Gardner 3Department of Geography, King's College, London, WC2, England Search for other works by this author on: GSW Google Scholar Geology (1980) 8 (7): 318–322. https://doi.org/10.1130/0091-7613(1980)8<318:CTAPI>2.0.CO;2 Article history 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 Peter A. Bull, Stephen J. Culver, Rita Gardner; Chattermark trails as paleoenvironmental indicators. Geology 1980;; 8 (7): 318–322. doi: https://doi.org/10.1130/0091-7613(1980)8<318:CTAPI>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 Crescentic markings on the surface of quartz and garnet grains have recently been considered as suitable indicators of paleoenvironment, particularly glacial modification. A review of the literature suggests that other mechanisms can cause similar features. Considerable caution is advised when using these chattermark trails as one-step indicators of glaciation. 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.