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Talus slopes form in environments characterized by steep terrain, where the angle of repose of loose rock and debris is exceeded. Conditions that favor their formation include frequent freeze-thaw cycles, which promote rock fragmentation, as well as weathering processes that loosen material. Additionally, the presence of vegetation can stabilize slopes, but in its absence or due to disturbances, loose material can accumulate at the base of cliffs, creating talus slopes.

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14h ago

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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 talus?

Talus is rock debris at the bottom of a slope.


Which type of mass wasting produces a talus slope?

fall


What is talus slope and how is it formed?

Talus slopes are broken rocks formed by gravity and the convergent boundary. Ex: Devils Lake Gorge.


Where would you expect to find talus?

You would expect to find talus at the base of a cliff or steep slope. Talus consists of loose, fragmented rock debris that has accumulated from the erosion of the cliff or slope above. It often forms a slope of angular rocks and boulders created by gravity pulling the rock fragments downhill.


Material that collects at the foot of a steep slope or cliff is called?

Talus


What is another word for sloping hill?

Incline, slope, gradient, talus...


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

Scree or Talus .


What is a talus on a medieval castle?

A slope on the wall to prevent siege towers and ladders


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.


How is a talus cone produced?

A talus cone is produced through the accumulation of rock debris and sediment that has fallen from a steep slope or cliff. This material, often called talus, collects at the base of the slope due to gravity, forming a conical shape as it piles up over time. The angle of repose, which is the steepest angle at which the debris remains stable, influences the cone's slope. Natural processes such as weathering and erosion contribute to the continuous supply of material to maintain the talus cone.


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)