These are known as scree or talus.
fragments
Physical weathering breaks rocks into smaller pieces without changing their chemical composition. This process occurs through mechanisms such as freeze-thaw cycles, thermal expansion, and abrasion from wind or water. The resulting fragments can then be further broken down by chemical weathering or transported by erosion. Ultimately, physical weathering contributes to soil formation and landscape changes.
Water can get into fractures/joints/pores of rock, freeze, and then expand, weathering the rock.
it does
Freeze/thaw cycles expand existing fissures in existing rock by the expansion caused by ice crystal formation. This leads to further erosion of the rock by freeze/thaw and chemical weathering from rainwater.
The mechanical weathering caused by rock fragments tumbling against each other is called abrasion. This process can lead to the wearing down and smoothing of the rock surfaces involved.
No, weathered rock fragments can vary in size depending on the type of weathering that occurs. Mechanical weathering can break rocks down into different sizes, forming a mixture of small and large fragments. Chemical weathering can also cause rocks to disintegrate into varying sizes based on the mineral composition and the intensity of the weathering process.
The type of weathering in which rock is physically broken into smaller pieces is called mechanical weathering. This process occurs without any change in the rock's chemical composition and can result from factors such as temperature changes, freeze-thaw cycles, or the action of wind and water. As rocks break down into smaller fragments, they become more susceptible to further weathering processes.
Freeze/thaw cycles are an example of mechanical weathering of rock.
The forces of mechanical weathering include frost wedging (freeze-thaw cycles), root wedging (roots growing into cracks), abrasion (rock-on-rock friction), and pressure release (rock expansion due to removal of overlying material). These forces break down rocks into smaller fragments over time.
Freeze-thaw weathering occurs when water seeps into cracks in rocks, freezes, expands, and breaks the rock apart. Over time, this process weakens the rock, causing it to fragment and break into smaller pieces. The repeated cycles of freezing and thawing can lead to the formation of scree slopes as the broken rock fragments accumulate at the base of steep slopes.
When water in the cracks in rocks freezes and expands, it can cause mechanical weathering known as freeze-thaw weathering. The expanding ice exerts pressure on the rock, which can eventually lead to the rock fracturing or breaking apart. Over time, repeated freeze-thaw cycles can contribute to the breakdown of rocks into smaller fragments.