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U-shaped is wrong that's what it says on my worksheet! the definiton of u shaped valleys are bowl like depressions!

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What are smaller glacial valleys that join the deeper main valley?

They are called hanging valleys. The smaller glacier valleys are the hanging walls that join the deeper main valley called the U-shaped valley.


Smaller glacial valleys that join the deeper main valley?

Smaller glacial valleys that join a deeper main valley are often referred to as tributary valleys or hanging valleys. These valleys typically form when smaller glaciers flow into a larger glacier, resulting in a steep drop-off where the tributary meets the main valley. As the main glacier erodes the landscape, it carves out a deeper trough, leaving the smaller valleys elevated, which can create stunning waterfalls when the tributary streams plunge into the main valley below. This geological feature is common in mountainous regions shaped by glacial activity.


How are hanging vallies formed?

Hanging valleys are formed when smaller glaciers flowing from tributary valleys join a larger glacier in a main valley. As the larger glacier is more powerful, it erodes the main valley deeper than the tributary valleys. This results in the tributary valleys being left at higher elevations once the glaciers retreat, creating the characteristic "hanging" appearance.


What are the erosional features you might expect to see in an area where valley glaciers exist or have existed?

Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.


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