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The general term for material that falls down and gathers at the foot of a steep cliff or mountain face is scree.
Scree or Talus .
Talus
the slope.
Cuz it called that =D
This may be known as a scree slope or a talus pile. Talus and scree are normally used interchangeably, however scree normally refers to material of gravel size or smaller and talus to larger debris.
The rock fragments that accumulate at the base if a steep slope are usually known as scree or talus.
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.
The general term for material that falls down and gathers at the foot of a steep cliff or mountain face is scree.
The general term for material that falls down and gathers at the foot of a steep cliff or mountain face is scree.
Scree or Talus .
A slope of unconsolidated slope of granite gravels would be called a scree slide. The toe of such a slope would be known as the 'talus' - a word meaning ankle. And thus referring to the gentle curve.
A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.
Those letters will spell scree (loose stones that cover a slope).
A slump
Talus
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.