Outwash & Till
Stalagmites and stalactites are two features formed by underground deposition. Stalactites hang from the ceiling of caves and are formed as mineral-rich water drips down and leaves behind deposits of minerals. Stalagmites, on the other hand, form on the cave floor as the dripping water deposits minerals and builds up over time.
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.
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.
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.
A) glacial deposits
what is a ridge formed from deposits are
Glacial deposits or glacial drift refer to all sediments of glacial origin. These deposits include materials such as till, moraines, outwash plains, and glacial erratics that are left behind by the movement of glaciers.
A kettle is a depression left by melted blocks of ice in glacial deposits.
till is the name of the material. In most cases all glacial-related deposits are unsorted and unstratified.
glacial deposits
hanging valley
it will be D.outwash
Krzysztof Brodzikowski has written: 'Glacigenic sediments' -- subject(s): Glacial landforms, Sediments (Geology), Glacial deposits, Glacial epoch
No, one they are used they can't come back.
ALLSLWE
Glacial deposits are found in Africa, India, and Australia because these regions were once covered by ice sheets during past glacial periods. The movement of glaciers transported rocks, sediments, and other materials across these continents, leaving behind distinct glacial deposits like till, moraines, and erratics. These deposits serve as evidence of the Earth's past climate history and the presence of glaciers in regions where they are uncommon today.