alpine glaciers
Cirques are the rounded basins carved into the sides of mountains by valley glaciers. They are typically characterized by steep walls and a bowl-like shape. The process of glacial erosion forming cirques is known as plucking and abrasion.
Ussually by three cirques A cirque is an origin point for glaciers in mountainous areas. It is a deep depression with three high walls and an open area from which the glacier moves forward, down the mountain side. Over time, as rock is eroded, these become wider and deeper. A mountain horn, such as the Matterhorn in the Alps forms when a peak is surrounded on two or more sides by cirques. As the cirques expand and rock is eroded the peak is honed into a point, forming a horn.
Alpine Glacier produce a variety of erosional features. These features are usually rounded or polished grooves made by the glacier's passing. The features are called arete, Circque, horn, tarn, u shaped valley, and hanging valleys.
Yes. A continental glacier spreads around all sides, while the valley glaciers spread along it's length.
The steps that are built into the sides of the mountains are called terraces. It makes it so that farmers can grow more crops and be able to reach them as well. The correct term for it would be terrace farming. It's one of those little engineering quirks that the Chinese have developed over many years.
Cirques are the rounded basins carved into the sides of mountains by valley glaciers. They are typically characterized by steep walls and a bowl-like shape. The process of glacial erosion forming cirques is known as plucking and abrasion.
A cirque is the top of a glacier valley.
Ussually by three cirques A cirque is an origin point for glaciers in mountainous areas. It is a deep depression with three high walls and an open area from which the glacier moves forward, down the mountain side. Over time, as rock is eroded, these become wider and deeper. A mountain horn, such as the Matterhorn in the Alps forms when a peak is surrounded on two or more sides by cirques. As the cirques expand and rock is eroded the peak is honed into a point, forming a horn.
Land features formed from ice erosion include cirques, u-shaped valleys, and fjords. Cirques are bowl-shaped depressions at the head of a glacier, u-shaped valleys are deep valleys with steep sides carved out by glaciers, and fjords are long, narrow inlets with steep cliffs created by glaciers flowing into the sea.
Alpine Glacier produce a variety of erosional features. These features are usually rounded or polished grooves made by the glacier's passing. The features are called arete, Circque, horn, tarn, u shaped valley, and hanging valleys.
Moraine
Cirques: bowl-shaped hollows formed at the head of a glacier where snow and ice accumulate. Moraines: ridges of glacial debris, such as rocks and sediment, deposited along the sides or at the terminus of a glacier. U-shaped valleys: valleys carved by glaciers that have distinctive steep sides and flat bottoms.
The sharp pyramid-shaped peak formed by the erosion of three or more cirques on a mountain is called a horn. This landform is typically created by the intersection of multiple glaciers eroding the mountain from different sides, resulting in steep, jagged peaks. Famous examples include the Matterhorn in the Swiss Alps.
Not always but
Glaciers are the main agents of erosion that create U-shaped valleys. As glaciers move downhill, they carve out the valley floor and sides through the process of abrasion and plucking. The unique U-shape is a characteristic feature of valleys that have been shaped by glaciers.
Waterfalls on the sides of mountains reveal much about hydrology.
The four major types of landforms found on Earth are mountains, plains, plateaus, and valleys. Mountains are elevated landforms with steep sides, while plains are flat expanses of land with minimal elevation changes. Plateaus are elevated flatlands, often with steep cliffs on one or more sides. Valleys are low-lying areas between hills or mountains, often carved by rivers or glaciers.