scabland वाक्य
उदाहरण वाक्य
मोबाइल
- This plant is restricted to scabland habitat with exposed bedrock.
- It is an indicator of scabland habitat.
- The deluge stripped away soil, cut deep canyons and carved out of earth, leaving behind areas of stark scabland.
- Examples of scabland features, such as large kolk-excavated potholes, provide evidence of the tremendous powers of the floods.
- One commonly cited example is the Channeled Scabland of Washington State; it was formed by the breakout of water from the Pleistocene Lake Missoula.
- There is a unique character to the Drumheller Channels; unlike most other Channeled Scabland zones, no single centralized channel or major cataracts were formed.
- The creek parallels the adjacent Cow Creek scabland and joins the Palouse River just before it departs Washtucna Coulee, the abandoned flood-scoured course of the river.
- On June 5th 1923, Moultray argued that his birthplace which he called the Channeled Scabland, was the product of a cataclysmic flood, which he called the Spokane flood.
- "' Rock Lake "'is the deepest and largest of all scabland lakes left behind from the Missoula Floods, and holds that distinction for all of eastern Washington.
- The presence of Middle and Early Pleistocene Missoula flood deposits have been documented within the Channeled Scabland as other parts of the Columbia Basin, e . g . the Othello Channels, Columbia River Gorge, Quincy Basin, Pasco Basin, and the Walla Walla Valley.
- The Touchet beds are one element in a chain of evidence which helped identify and define the progression of the Missoula Floods, which occurred around 16, 450 to 13, 750 years scabland regions north of Lake Lewis, and redeposited them in pronounced layers before receding.
- In addition, Middle and Early Pleistocene Missoula flood deposits have been documented to comprise parts of the glaciofluvial deposits, informally known as the " Hanford formation " that are found in parts of the Othello Channels, Columbia River Gorge, Channeled Scabland, Quincy Basin, Pasco Basin, and the Walla Walla Valley.
- Within the Columbia Basin, detailed investigation of the Missoula floods'glaciofluvial deposits, informally known as the " Hanford formation ", has documented the presence of Middle and Early Pleistocene Missoula flood deposits within the Othello Channels, Columbia River Gorge, Channeled Scabland, Quincy Basin, Pasco Basin, and the Walla Walla Valley.
- The controversy whether the Channeled Scabland landforms were formed mainly by multiple periodic large floods or by a single grand-scale cataclysmic flood from either late Pleistocene Glacial Lake Missoula or an unidentified Canadian source reappeared in 1999 . Shaw s team reviewed the sedimentary sequences of the Touchet beds and concluded that the sequences do not automatically imply multiple floods separated by decades or centuries.
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