glacial outwash वाक्य
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- The "'Pakhuis Formation "'tillite ( a lithified glacial outwash gravel ) occurs on the highest point of Table Mountain, at Maclear's Beacon and on parts of the Hottentots-Holland range.
- The terrace was formed by glacial outwash coming down the Hocking River, which became dammed at The Plains and found a new outlet to the northeast, leaving the terrace in place.
- The fairly shallow average depth of 78 feet ( 24 m ) of today's Long Island Sound is the result of fine lake-bottom sediments deposited as glacial outwash slowed in Lake Connecticut.
- As the water moved through either Lake Agassiz or other proglacial lakes, they completely trapped and removed any glacial outwash and the older, reworked organic material and reworked nanofossils that the outwash contained.
- Typical Puget Sound profiles of dense glacial till overlying permeable glacial outwash of gravels above an impermeable bed of silty clay may become unstable after periods of unusually wet weather and slump in landslides.
- Effie died in 1963, and Fred arranged to sell the house and surrounding acreage of Garry oak woodland and glacial outwash prairie to the Washington State Game Department ( now the Washington Department of Fish & Wildlife ).
- The site is listed in the Geological Conservation Review because it consists of a complex sequence of Pleistocene sediments, including coarse glacial outwash gravels at the base overlain by a complex sequence of interglacial freshwater, estuarine and marine sands.
- The formation of Kaitorete Barrier began at the end of the Last Glacial Maximum 20, 000 years ago valley glaciers advanced in Canterbury and subsequent glacial outwash rivers delivered vast quantities of sand, gravel and silt to the coast.
- Originally, 12, 000 13, 000 years ago, this was the glacial outwash channel that drained water away from the glacier westward, northward and finally eastward into the Atlantic some distance from where Route 6A ( Truro Center Road ) now passes.
- Opening of an ice-free corridor did not occur until after 13k to 12k cal years BP . The early environment of the ice-free corridor was dominated by glacial outwash and meltwater, with ice-dammed lakes and periodic flooding from the release of ice-dammed meltwater.
- Nearby is the Kenn Church, Kenn Pier & Yew Tree Farm SSSI, a geological Site of Special Scientific Interest which is listed in the Geological Conservation Review because it consists of a complex sequence of Pleistocene sediments, including coarse glacial outwash gravels at the base overlain by a complex sequence of interglacial freshwater, estuarine and marine sands.
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