A scree is when water in mountains freeze and cracks the mountain, scree is crushed bits of rock.
Often barely at rest angle.
scree
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.
A huge sloping heap of scree suggests that there are frequent frost/thaw cycles, which cause rocks to break loose from the cliff face and collect at the base. This indicates cold temperatures, moisture, and potentially high winds, contributing to the ongoing erosion and accumulation of loose rock.
SCREE or TALUS.
Scree, gravel, talus.
what is scree element
scree
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.
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.
Both scree and talus are a collection of broken rock fragments, such as at the foot of a cliff. Scree has smaller fragments- about golf ball sized, where talus is a bigger chunk of broken rock. "The footing was very poor when crossing over the field of scree." Think of a pile of big gravel.
That heavy tobbogan I'd been dragging along was quite handy when our progress seemed to be halted by the swath of scree in our path. That toboggan careened wildly as we screamed down the scree. Unless my life depends upon it, I'll never ride another toboggan down the scree.
Scree
scree
One can find scree all over the world. Scree refers to fragments of broken rocks which are found at the base of mountains, volcanoes, and valleys due to rockslides. These terrain features can be found on nearly every continent and country.
Penelope Ann Crompton has written: 'Scree development on Eaffin Island' -- subject(s): Rock slopes, Scree
A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.
Higher altitudes may have a greater impact on the formation of scree as the freeze-thaw cycle is more pronounced in colder temperatures, leading to more frequent rock fragmentation. Additionally, increased wind and precipitation at higher altitudes can contribute to the breakdown of rocks into scree material.