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Scree or Talus .
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.
The general term for material that falls down and gathers at the foot of a steep cliff or mountain face is scree.
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.
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.
what is scree element
It's scree, next time try Dictionary.com :)
Scree slopes are common in upland areas, such as the Lake District. The scree - broken fragments of rock - is usually formed by freeze-thaw activity. This breaks solid rock into smaller, often angular particles. Scree is common in mountainous areas, since night-time temperatures often fall below freezing point, and there is a ready supply of moisture to freeze. A typical lowland glaciated valley can be seen in the background. Scree slopes are common in upland areas, such as the Lake District in northwest England. The scree, broken fragments of rock, is usually formed by freeze-thaw activity. This breaks solid rock into smaller, often angular particles. They are common in mountainous areas, since night-time temperatures often fall below freezing point, and there is a ready supply of moisture. Scree slope and cliffs near Eldborg, an ancient volcanic crater, in southern Iceland. Rocks fractured and broken apart by freeze-thaw action here form slopes of loose material. The slopes are very similar to the landscape of hot desert areas. Areas such as southern Iceland - which are called periglacial (literally on the edge of glacier activity) - are sometimes called cold deserts. Pile of rubble and sediment that collects at the foot of a mountain range or cliff. The rock fragments that form scree are usually broken off by the action of frost (freeze-thaw weathering). With time, the rock-waste builds up into a heap or sheet of rubble that may eventually bury even the upper cliffs, and the growth of the scree then stops. Usually, however, erosional forces remove the rock waste so that the scree stays restricted to lower slopes.
It is mostly found at the bottom base of cliffs , mountain cliffs , volcanoes or valley shoulders