Portal de Periódicos da CAPES

Relations of Caliche to Small Natural Depressions, Southern High Plains, Texas and New Mexico

1971; Geological Society of America; Volume: 82; Issue: 7 Linguagem: Inglês

10.1130/0016-7606(1971)82[1983

1943-2674

C. C. Reeves,

Aeolian processes and effects

Research Article| July 01, 1971 Relations of Caliche to Small Natural Depressions, Southern High Plains, Texas and New Mexico C. C REEVES, JR. C. C REEVES, JR. Department of Geosciences, Texas Tech University, Lubbock, Texas 79409 Search for other works by this author on: GSW Google Scholar Author and Article Information C. C REEVES, JR. Department of Geosciences, Texas Tech University, Lubbock, Texas 79409 Publisher: Geological Society of America Received: 12 Feb 1971 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1971, 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 (1971) 82 (7): 1983–1988. https://doi.org/10.1130/0016-7606(1971)82[1983:ROCTSN]2.0.CO;2 Article history Received: 12 Feb 1971 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation C. C REEVES; Relations of Caliche to Small Natural Depressions, Southern High Plains, Texas and New Mexico. GSA Bulletin 1971;; 82 (7): 1983–1988. doi: https://doi.org/10.1130/0016-7606(1971)82[1983:ROCTSN]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 Most small natural depressions on the southern High Plains were produced by deflation or depositional irregularities of Pleistocene sand sheets, thus bear no genetic relation to the underlying Pliocene "caprock" caliche. Other small depressions have probably been produced by animals. The number of small depressions which reflect sinks in the underlying caliche is unknown. 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.