WebMay 6, 2024 · Four examples of glacial sediments are shown here. Describe the important characteristics (e.g., sorting, layering, grain-size range, grain shape, sedimentary structures) of each one and give each a name (choose from glaciofluvial, glaciolacustrine, lodgement till, ablation till, and glaciomarine). Figure A WebBecause ice is plastic when deformed slowly and under pressure, the glacial ice flows downhill like a slow river of ice. Creep is this movement by deformation. Glide is a rigid-body motion of the glacier as it slides down on a bed surface, usually lubricated by meltwater that flows between the bedrock and the underside of the glacier.
What are crevasses in glaciers? - todai.youramys.com
WebNov 16, 2024 · Crevasses are fractures in a glacier caused by the stresses of movement. They are like the cracks in the surface of clay as one pulls it apart past the limits of elasticity. They most often occur where the flow of a glacier increases, like in a steep deepening valley, and are thus oriented perpendicular to direction of flow. Web0.34 pts Question 4 What process would you expect to see in the accumulation zone of a glacier? till deposition a terminal moraine outwash plains glacial erosion 0.34 pts … green carpet cleaning monterey colorado
crevasse - National Geographic Society
WebWhy do crevasses form in the top of a glacier? A crevasse is a crack in the surface of a glacier caused by extensive stress within the ice. For example, extensive stress can be caused by stretching if the glacier is speeding up as it flows down the valley. Crevasses can also be caused by the ice flowing over bumps or steps in the bedrock. WebScore: 4.3/5 (8 votes) . Crevasses usually form in the top 50 meters (160 feet) of a glacier, where the ice is brittle.Below that, a glacier is less brittle and can slide over uneven surfaces without cracking. The inflexible upper portion may … WebSediments and rocks fall off the cliffs surrounding the glacier and move through crevasses to the base of the glacier. Sediments and rocks are deposited on glaciers by streams that flow into the glaciers. Sediments and rocks form on top of the glaciers through lithification O Sediments and rocks are plucked off Show transcribed image text green carpet cleaning kauai