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What cross valley profile is typical of canyons and valleys eroded and deepened by alpine or valley glaciers?
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
What cross-valley profile is typical of canyons and valleys eroded and deepened by alpine or valley glaciers?
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
Difference in shape of a typical stream carved valley compared to a typical glacial carved valley?
A stream-carved valley typically has a V-shape with a narrower and deeper profile due to the erosive force of flowing water. In contrast, a glacial-carved valley has a U-shape with a wider and shallower profile due to the movement of glaciers scooping out the landscape.
What erodes broad U shaped Valleys in mountain rivers valleys?
Glaciers are primarily responsible for eroding broad U-shaped valleys in mountain river valleys. As glaciers move downhill, they carve out wide and deep valleys due to their erosive power. The U shape is created as the glacier erodes the rock and sediment below it, creating a distinct profile with steep sides and a flat bottom.
What is the differences between v-valley and u-valley?
V-valley refers to a type of valley on a topographic map that has a V-shaped profile, typically formed by erosion from a river or stream. U-valley refers to a valley with a U-shaped profile, typically formed by glacial erosion. V-valleys are more narrow and have steeper sides compared to U-valleys.
How deep is a typical valley?
There is no "typical" valley depth - valleys can range from a depth of only a few feet to hundreds of feet deep depending upon the weathering and erosion taking place in the valley.
Are glacial valleys you shaped?
Yes, glacial valleys are often U-shaped due to the erosion caused by glaciers. As glaciers advance, they scoop out and widen valleys, resulting in a distinct U-shaped profile. This glacial erosion process leaves behind characteristic features like steep sides and flat bottoms.
What erodes bored you shaped valleys in mountain river valley?
Bored or U-shaped valleys in mountain river valleys are primarily formed by glacial erosion. As glaciers advance, they carve out the landscape, widening and deepening valleys through the process of abrasion and plucking. This results in the characteristic U-shape, contrasting with V-shaped valleys formed by river erosion. Over time, the immense weight and movement of the glacier reshape the terrain, leading to the distinctive valley profile.
What landforms are typical int the west indies?
Typical landforms in the West Indies include volcanic mountains, coral reefs, limestone caves, and sandy beaches. The region also has valleys, plains, and coastal cliffs.
What is a long valley profile?
A long valley profile shows the cross-sectional view of a valley from its headwaters to its mouth. It typically displays the variations in elevation and slope along the length of the valley, often revealing features such as V-shaped valleys, interlocking spurs, and river meanders. This profile is useful for analyzing the geological and geomorphological history of a valley.
What is evidence that a glaciers was at?
Presence of glacial striations, moraines, and glacial valleys are evidence that a glacier was there. These features are formed by the movement and deposition of ice, rocks, and sediment as the glacier advances and retreats. Additionally, erratic boulders, cirques, and U-shaped valleys are also typical evidence of past glacial activity.
What is the plural form of the valley?
The plural form is valleys.
