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)
At the bottom of a cliff.
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.
Scree, gravel, talus.
magnetic field.
Talus slopes are broken rocks formed by gravity and the convergent boundary. Ex: Devils Lake Gorge.
Talus Field's are A BUNCH OF ROCKS. They're all oddly shaped. They don't do anything. ANYTHING AT ALL. pce out.
The talus (ankle bone) articulates (moves interactively) with both the tibia and fibula, the bones of the lower leg.
Talus
Talus
The talus bone.
Talus
The distal tibia and fibula both articulate with the talus. The talus is the superiormost of the tarsals.
Talus is rock debris at the bottom of a slope.
Mudflows canot deposit talus. By definition a talus deposit is composed of broken rock depoited by gravity.
Talus-Saint-Prix's population is 84.
The common name for talus is ankle. Tal- is the related medical terminology combining form.