Last edited by Moll
Sunday, May 3, 2020 | History

2 edition of Windust phase in Lower Snake River region prehistory found in the catalog.

Windust phase in Lower Snake River region prehistory

Rice, David G.

Windust phase in Lower Snake River region prehistory

by Rice, David G.

  • 145 Want to read
  • 24 Currently reading

Published by Laboratory of Anthropology, Washington State University in Pullman .
Written in English

    Subjects:
  • Excavations (Archaeology) -- Snake River Valley (Wyo.-Wash.),
  • Indians of North America -- Antiquities

  • Edition Notes

    Statementby David G. Rice.
    SeriesReport of investigations - Laboratory of Anthropology, Washington State University ; no. 50, Reports of investigations (Washington State University. Laboratory of Anthropology) -- no. 50.
    ContributionsWashington State University. Laboratory of Anthropology,
    The Physical Object
    Paginationxii, 225 leaves :
    Number of Pages225
    ID Numbers
    Open LibraryOL16413817M

    Unearth the geological wonders of Idaho’s Snake River Plain, a land shaped by volcanic eruptions and mega-floods among other powerful forces of nature. Marvel at Shoshone Falls, and discover dramatic formations at City of Rocks National Reserve. On a whitewater rafting trip, learn the history of lava flows and the Bliss Landslide. Course. The river begins at Lake Doré in North Algona-Wilberforce township. It flows east under Ontario High then south past the community of Lake then turns east, takes in the right tributary Mink Creek, travels through the Upper Osceola Marsh, and reaches the community of Osceola in Admaston–Bromley township. It heads north through the Snake River Marsh, a proposed Country: Canada.

    HISTORY OF SNAKE RIVER CANYON INDICATED BY REVISED STRATIGRAPHY OF SNAKE RIVER GROUP NEAR HAGERMAN AND KING HILL, IDAHO By HAROLD E. MALDS Snake River of that time, as far downstream as Bliss, flowed (which is the local name for the lower reach of the Big Wood River) showed that the Mc­ Kinney overlies the Wendell Grade. Because both theCited by: 4. American Antiquity Randolph, Joseph E., and Max Dahlstrom Archaeological test excavations at Bernard Creek Rocksheiter. University of Idaho Anthropological Research Manuscripts Series No. Moscow, Idaho. Rice, David G. The Windust phase in lower Snake River prehistory. Report of Investigations No. Cited by: Lower Monumental Dam is 3, feet long, making it the longest dam of the four dams completed along the Lower Snake River between and During its construction, it escaped many -- though not all -- of the environmental protests that accompanied the .

      The southern terminus of the Columbia Plateau surveys the stark, scalloped Snake River country of southeast Washington. Pioneer John Mullan scratched out a wagon road here in the middle of the 19th century; the rail line sometimes runs on top of the old wagon road, sometimes paralleling it, offering an added bit of history/5(10). through a brief summary of the region’s prehistory and history. The INEL itself is central to the area of study and is representative of many, though not all, Figure Cultural areas adjacent to the eastern Snake River Plain (hatched area) (from Reed et al. ). aspects of the region’s ecology as it . (CNN) -- The U.S. Army Corps of Engineers wants to know how the removal of four dams along the Lower Snake River would affect endangered salmon and steelhead runs, and the region's economy.


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Windust phase in Lower Snake River region prehistory by Rice, David G. Download PDF EPUB FB2

SyntaxTextGen not activatedProposed Pdf Typology for the Lower Snake River Region, Southeastern Washington. Frank C. Leonhardy, David G. Rice. (tDAR id: ) This Resource is Part of the Following CollectionsCited by: External links modified.

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I made the following changes.Snake River, largest tributary ebook the Columbia River and one of the most important streams in the Pacific Ebook section of the United rises in the mountains of the Continental Divide near the southeastern corner of Yellowstone National Park in northwestern Wyoming and flows south through Jackson Lake along the eastern base of the Teton Range in Grand Teton National Park.