Currents of Great Salt Lake, Utah

Utah Geology Pub Date : 1975-01-03 DOI:10.34191/ug-2-2_103
W. Katzenberger, J. A. Whelan
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引用次数: 2

Abstract

The chief factor controlling currents in Great Salt Lake is inflow. In the south arm inflow from Bear River and from Farmington Bay sets up two major counterclockwise currents. In the north arm, flow through culverts in the Southern Pacific Railroad causeway induces two major northwest-flowing currents. Currents in Great Salt Lake caused by winds are rare and diminish rapidly.
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犹他州大盐湖的水流
控制大盐湖水流的主要因素是入流。在南臂,来自贝尔河和法明顿湾的流入形成了两个主要的逆时针流。在北岸,流经南太平洋铁路堤道涵洞的水流形成了两股向西北方向流动的水流。大盐湖由风引起的海流很少见,而且会迅速减少。
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Currents of Great Salt Lake, Utah Sedimentary Cycles in the Nugget Sandstone, Northeastern Utah Largest Known Landslide of Its Type in the United States- A Failure by Lateral Spreading in Davis County, Utah Primary and Secondary Sedimentary Structures in Oil Shale and Other Fine-grained rocks, Green River Formation (Eocene), Utah and Colorado Bibliography of Utah Geology 1973
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