A.FjordsD Piles of rocksB.Horn peaksC Cracks in glaciersC.CrevassesA Steep cliffsD.Terminal morainesB Where cirques intersect
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Cirque: A bowl-shaped depression on the side of a mountain, formed by the erosive activity of a glacier. Cirques are typically characterized by steep walls and may contain a small lake called a tarn at their base.
Two types of glacial deposits are moraines, which are formations of mixed sediment pushed by and deposited from a glacier, and drumlins, which are elongated hills made of glacial till that form parallel to the direction of ice flow.
Yes, glacial troughs are U-shaped valleys that form through the erosion of moving glaciers. They have steep, straight sides and a flat bottom that was carved out by the glacier over time. The presence of a glacial trough indicates past glaciation in an area.
A fjord is a narrow bay that is formed by tectonic processes like plate movements, and later modified by glacial action through erosion and deposition of sediments. Fjords are typically found in regions that have experienced both tectonic and glacial activity, such as Norway and New Zealand.
The glacial features that occur in swarms of long and smooth canoe-shaped hills are called drumlins. Drumlins are typically formed under moving glaciers and indicate the direction of ice flow. They are important indicators of past glacial activity and can be found in large numbers clustered together in areas that were once covered by ice sheets.
Yes you can prevent glacial erosion. In an experiment in Italy, they put a white sheet of fleece the size of football fields over the glaciers. The glacier under the fleece blanket is melting much more slowly than the ice that is not covered by it.
hanging valley
Glacial drift
what is a landscape feature created by glacial deposits
A moraine is a landscape feature created by glacial deposits. Moraines are formations of unsorted rock debris that were transported and deposited by a glacier as it moved and melted. They can be found in various forms such as terminal moraines at the end of glaciers or lateral moraines along their sides.
Central Park in Manhattan was formed primarily as a result of glacial deposition during the last ice age. The park's landscape features, such as its hills, valleys, and rock formations, were sculpted by the movement of glaciers and the debris they left behind.
Striations would most likely form on the surface of the bedrock under the glacial ice. Striations are caused by the movement of large rocks embedded in the base of a glacier scraping across the bedrock, resulting in long, parallel grooves being carved into the bedrock surface.
The most well-known glacial feature on Kelleys Island would be the Glacial Grooves, located on the north side of the island. They were protected in the 1880's by deed and are generally recognized as the best examples of glacial action in the U S. There are numerous areas of glacial scratching and scouring on the island as well. If you search "Kelleys Island glacial grooves" you'll find several online pictures.
A cirque, also known as a Cwm or Corrie, is a feature of glacial erosion, formed in a mountainside.
Long Island, which was formed by a glacial moraine (the leading edge of the glacier pushing rock, soil and sand).
ideal type
No, it's main feature -- Yosemite Valley -- was created due to glacial erosion.
The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine