A glacier retreats when more ice melts away during the summer than that which forms during the winter. The glacier reduces in size as the ice in the zone of wastage melts. The retreating glacial ice never actually flows backwards; the ice simply melts away faster than is replenished from new glacial ice formation in … See more Continental glaciers (ice sheets, ice caps) are massive sheets of glacial ice that cover landmasses. Continental glaciers are currently eroding deeply into the bedrock of Antarctica and Greenland. The vast ice sheets are … See more If the amount of glacial ice formation in the zone of accumulation equals the amount of melting in the zone of wastage, then the glacier does not advance or retreat. While the ice within the glacier continues to flow … See more The upper 50 meters of the surface of the glacier, where the ice does not undergo plastic deformation, is referred to as the zone of fracture. In … See more Glaciers have a snow budget, much like a monetary bank account. The more money deposited into a bank account, the larger the account grows. … See more Web1) climate must be cold enough that winter snow doesn't melt completely away 2) there has to be enough snowfall that a large amount can accumulate, even during the summer 3) the surface that the snow falls on must have a gentle slope so that snow doesn't slide, and it also needs to be protected from wind

7.10: Glacial Erosion - Geosciences LibreTexts

WebApr 16, 2024 · Valley glaciers can flow in all directions as they move, while continental glaciers move down slopes already cut by rivers. Valley glaciers cover much of a continent, while continental glaciers cover a small area of mountains. Continental glaciers are long and narrow, while valley glaciers are wider in size. WebJul 7, 2024 · Ice Flow: Glaciers move by internal deformation (changing due to pressure or stress) and sliding at the base. What are 2 different ways glaciers shape the land? There are three distinct ways that glaciers shape the land: 1) erosion 2) transportation and 3) deposition. Erosion picks up material through weathering through plucking and abrasion. flower shops in claysburg pa

Valley Glaciers - Geography Site

WebAs a glacier flows, weathering takes place on the land around it. The main weathering process is known as freeze-thaw weathering. This is where water, either rain water or … WebFeb 12, 2013 · In a way, glaciers are just frozen rivers of ice flowing downhill. Glaciers begin life as snowflakes. When the snowfall in an area far exceeds the melting that occurs … WebFeb 9, 2024 · Glaciers move by a combination of (1) deformation of the ice itself and (2) motion at the glacier base. At the bottom of the glacier, ice can slide over bedrock or … flower shops in clinton indiana