Glacial erosion gouges 'U' shaped (cross-section) of valleys, and deposit moraine (mounds of the rocks and debris) as they melt.
Ice erosion can create features such as cirques (bowl-shaped hollows on mountainsides), arêtes (sharp ridges between two cirques), and horns (sharp peaks formed by glaciers eroding multiple sides). These features are commonly found in glaciated mountainous areas.
when glacier melts , it deposits the sediment it eroded from the land, creating various landforms
Till, moraine, and kettle.
I dont know how to explain in good way.
It is simply sea caves, canyons, evened out shorelines, and abrision+collision=plucking and sea caves. That's the way that geographers and scientists think of it because this is just the easiest explanation of this term. Your welcome
Headlands, bays, sea caves, and sea stacks are four features formed by wave erosion along a coast. Headlands are rocky structures jutting out into the sea, while bays are curved inlets where the land recedes. Sea caves are hollowed-out spaces in coastal cliffs, and sea stacks are isolated rock pillars left behind from eroded cliffs.
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.
Plains are typically formed through weathering and erosion of existing landforms, such as mountains or plateaus, over long periods of time. Factors like water, wind, and ice gradually wear down the land, creating flat expanses of relatively low elevation. Geological processes like sediment deposition and tectonic activity can also contribute to the formation of plains.
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.
Mountains can be formed by erosion!
The Grand Canyon is a surface feature formed by water erosion. All riverbeds are formed by water erosion. Hoodoos are formed by water erosion.
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Hoodoos formed as a result of erosion by ice.
Some of the features of the California landscape formed as the result of tectonic processes that took place deep beneath the surface. Wind Water ice and Other agents of erosion at the surface carved other features of the landscape
Glacial Erosion formed Yosemite Valley and the Sierra Nevada
sand dunes
cave formations and sinkholes
Ice, as glaciers during the ice-ages, scoured mountains and formed 'U' shaped valleys.
Silting. Erosion.