Cover image for Late-Quaternary Environments of the United States : The Late Pleistocene.
Late-Quaternary Environments of the United States : The Late Pleistocene.
Title:
Late-Quaternary Environments of the United States : The Late Pleistocene.
Author:
Wright, H.E.
ISBN:
9780816655281
Personal Author:
Physical Description:
1 online resource (424 pages)
Contents:
Contents -- Contributors to This Volume -- Preface -- Introduction -- Glaciation -- 1. The Late Wisconsin Glacial Record of the Laurentide Ice Sheet in the United States -- 2. The Cordilleran Ice Sheet in Alaska -- 3. The Cordilleran Ice Sheet in Washington, Idaho, and Montana -- 4. Late Wisconsin Mountain Glaciation in the Western United States -- Nonglacial Environments -- 5. Late-Pleistocene Fluvial Systems -- 6. Depositional Environment of Late Wisconsin Loess in the Midcontinental United States -- 7. Sangamon and Wisconsinan Pedogenesis in the Midwestern United States -- 8. Trends in Late-Quaternary Soil Development in the Rocky Mountains and Sierra Nevada of the Western United States -- 9. The Periglacial Environment in North America during Wisconsin Time -- 10. Pluvial Lakes of the Western United States -- Coastal and Marine Environments -- 11. Sea Level and Coastal Morphology of the United States through the Late Wisconsin Glacial Maximum -- 12. The Ocean around North America at the Last Glacial Maximum -- Pleistocene Biota -- 13. Vegetational History of the Northwestern United States Including Alaska -- 14. Late Wisconsin Paleoecology of the American Southwest -- 15. Vegetational History of the Eastern United States 25,000 to 10,000 Years Ago -- 16. Terrestrial Vertebrate Faunas -- 17. Late Wisconsin Fossil Beetles in North America -- 18. The Antiquity of Man in America -- Climatology -- 19. Paleoclimatic Evidence from Stable Isotopes -- 20. Late-Pleistocene Climatology.
Abstract:
To many, the Pleistocene Epoch, which constitutes the earlier and major part of the Quaternary Period, is synonymous with the glacial ages and is viewed as a time of dramatic environmental change. Although there now is abundant evidence that glaciations occurred not only during the Pleistocene but through much of the Tertiary Period as well, and therefore are more appropriately considered as late-Cenozoic phenomena.
Local Note:
Electronic reproduction. Ann Arbor, Michigan : ProQuest Ebook Central, 2017. Available via World Wide Web. Access may be limited to ProQuest Ebook Central affiliated libraries.
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