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A sloping mass of rock fragments below a cliff called?

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.


What is scree?

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.


What material making up a scree slope is called?

The material making up a scree slope is called "scree" or "talus." It consists of loose rock fragments that have fallen from a cliff or steep slope, typically due to weathering and erosion processes. These angular pieces of rock accumulate at the base of the slope, forming a steeply angled deposit. Scree slopes are often unstable and can shift or move due to gravity and other environmental factors.


What is the effect of freeze-thaw in the mountains?

Freeze-thaw cycles in mountains can lead to physical weathering of rocks due to the expansion and contraction of water in cracks and crevices. This process can break down rock material, contributing to the formation of talus slopes and scree fields. Over time, freeze-thaw cycles can also influence slope stability and contribute to the erosion of mountain landscapes.


How does a mountain slope form?

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.


Is freeze thaw chemical weathering?

No. Chemical weathering is to do with acidic rain. This is a type of physical weathering, where it isn't the rainwater's ph, but the fact it freezes in cracks, expands, and prises the rock apart(creating a broken skyline or a scree slope). It occurs in damp areas where water is sometimes, not always below freezing.


What term describes an accumulation of angular rock fragments at the base of a steep bedrock slope or cliff?

Talus or scree is the term used to describe an accumulation of angular rock fragments at the base of a steep bedrock slope or cliff. This process is commonly associated with physical weathering and erosion.


What is a large pile of debris that forms at the base of a slope?

Scree or Talus .


What is a talus field and how is it formed?

Talus, also called scree, is a term given to an accumulation of broken rock fragments at the base of crags, mountain cliffs, or valley shoulders. Formation of scree or talus deposits results from physical and chemical weathering and erosional processes acting on a rock face. The predominant processes that degrade a rock slope include: Mechanical weathering by ice Chemical weathering by mineral hydration and salt deposition Thermal stresses (heating by the Sun and cooling at night) Topographic stresses (stress from the rock formation process) Biotic processes (plants wedging themselves in cracks and crevasses)


A pile of rock fragments at the base of a cliff is called a?

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.


Why are large scree slopes found under cliffs and mountainous areas?

A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.


What is the scrambled word for seeCr?

Those letters will spell scree (loose stones that cover a slope).