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Scree or Talus .
The general term for material that falls down and gathers at the foot of a steep cliff or mountain face is scree.
A mountain is a high, uplifted area with steep slopes. Mountains are large elevated area that rises from level ground. They are large and steep hills.
All depends on how deep the water is, and whether the bottom slopes.
composite volcano
A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.
Weathered rock fragments at the bottom of a hill are called scree. Scree formation is commonly attributed to the formation of ice within mountain rock slopes.
Penelope Ann Crompton has written: 'Scree development on Eaffin Island' -- subject(s): Rock slopes, Scree
It is called scree.
Heaps of frost-weathered rock fragments are known as scree or talus. They form when frost action causes rocks to fracture and break apart, creating a loose accumulation of debris at the base of cliffs or steep slopes. Scree can be found in mountainous and glaciated regions.
Scree is a collection of broken rock fragments found at the base of cliffs or steep rocky slopes. It is formed through the process of frost weathering, where water seeps into fractures in the rocks, freezes, and expands, causing the rocks to break apart and fall to the base of the slope.
HABITAT Often nests on steep, rough terrain with little or no vegetation, including lava flows and scree slopes
Scree or Talus .
One word you can use is scree.
Small loose stones at the bottom of a cliff are commonly referred to as scree. Scree is made up of loose rock fragments that have accumulated due to erosion and weathering processes. It can be unstable and make hiking or climbing difficult.
what is scree element
Freeze-thaw weathering occurs when water seeps into cracks in rocks, freezes, expands, and breaks the rock apart. Over time, this process weakens the rock, causing it to fragment and break into smaller pieces. The repeated cycles of freezing and thawing can lead to the formation of scree slopes as the broken rock fragments accumulate at the base of steep slopes.