A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
Similar to rivers, glaciers have tributaries. However as the main glacier erodes deeper into the valley, the tributary is left higher up the steep sides of the glacier. These U-shaped valleys ending with a water fall at the cliff-face are called hanging valleys.
When a river erodes the landscape, ridges of land form in its upper course which jut into the river. These are called interlocking spurs. A glacier removes these ridges leaving behind truncated spurs.
Follow this link:
http://www.bbc.co.uk/schools/gcsebitesize/geography/glaciation/glacial_erosionrev1.shtml
Its on bbbc bitesize glaciation. Its really helpful! and has lots of pictures.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.
A hanging valley is the result of a glacier gouging a valley into the path of a larger glacier, much as tributary to a river would. The larger glacier carves out a deeper valley than the smaller tributary glacier and so the smaller valley is not as deep as the main valley and is said to hang.
It's called a "hanging valley". Many waterfalls occur at hanging valleys.
hanging valley
hanging valley
A hanging valley is a destructive force. This is because the valley is formed by erosion, anything that is causes elevation to fall is destructive.
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The Hanging Valley was created in 1989.
A hanging valley is a destructive force. This is because the valley is formed by erosion, anything that is causes elevation to fall is destructive.
It's called a "hanging valley". Many waterfalls occur at hanging valleys.
It's called a "hanging valley". Many waterfalls occur at hanging valleys.
They are called hanging valleys. The smaller glacier valleys are the hanging walls that join the deeper main valley called the U-shaped valley.
hanging valley
A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.
A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.
A rift valley forms when the lithospheric stretches, tension stress occurs, causing rock to pull apart, break, and form normal faults.s the hanging wall of a normal fault slide down the footwall, a long, flat, narrow rift valley forms.
Mountain, plateau, valley, hanging valley, ridge, spur, terrace, landslip.
hanging valley
A hanging valley is a destructive force. This is because the valley is formed by erosion, anything that is causes elevation to fall is destructive.