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- W2018666509 abstract "Research Article| December 01, 2005 Age and effects of the Odessa meteorite impact, western Texas, USA Vance T. Holliday; Vance T. Holliday 1Department of Anthropology and Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar David A. Kring; David A. Kring 2Lunar and Planetary Sciences and Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar James H. Mayer; James H. Mayer 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar Ronald J. Goble Ronald J. Goble 4Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Vance T. Holliday 1Department of Anthropology and Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA David A. Kring 2Lunar and Planetary Sciences and Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA James H. Mayer 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Ronald J. Goble 4Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588, USA Publisher: Geological Society of America Received: 20 May 2005 Revision Received: 27 Jul 2005 Accepted: 10 Aug 2005 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2005) 33 (12): 945–948. https://doi.org/10.1130/G21884.1 Article history Received: 20 May 2005 Revision Received: 27 Jul 2005 Accepted: 10 Aug 2005 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Vance T. Holliday, David A. Kring, James H. Mayer, Ronald J. Goble; Age and effects of the Odessa meteorite impact, western Texas, USA. Geology 2005;; 33 (12): 945–948. doi: https://doi.org/10.1130/G21884.1 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 The Odessa meteorite craters (Texas, United States) include a main crater (∼160 m diameter, ∼30 m deep) plus four smaller meteorite craters. The main crater was sampled by coring (to 22 m depth) to better understand its origin and history. Dating by optically stimulated luminescence indicates that it was produced immediately prior to ca. 63.5 ± 4.5 ka. Sediment filling the crater includes impact breccias produced at the time of impact; wind-dominated silts with minor amounts of pond sediments deposited ca. 63.5 ka, probably just after the impact, and ca. 53 ± 2 ka; wind-dominated silt ca. 38 ± 1.7 ka; and playa muds with a wind-blown silt component younger than 36 ka. The environment was arid or semiarid at the time of impact based on characteristics of soils on the surrounding landscape. The impact caused severe damage within 2 km and produced >1000 km/hr winds and thermal pulse. Animals within a 1–1.5-km-diameter area were probably killed. This is only the second well-dated Pleistocene hypervelocity impact crater in North America. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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