Erosion, or deformation. The water will slowly chip off the bits of lose rock. Deformation is when tectonic plates collide causing bending, or folding in the crust. The same for Covergent Boundries, when plates collide, Divergent Boundaries, when plates pull apart, and then Transform Boundaries, like the San Andreas fault. It took me 15 days to learn this, you 30 seconds. ! :)
The type of rock formed when weathering, deposition, and cementation are all involved is sedimentary rock. Weathering breaks down rocks into sediments, which are then transported and deposited by water, wind, or ice. Cementation occurs when minerals precipitate and bind the sediments together to form solid rock.
The type of weathering that does not alter the chemical composition of the rock is called physical weathering. The acid weathering usually alter the chemical composition of a rock.
Through the process of metamorphism, a rock can be subjected to high temperatures and pressures, causing its mineral composition and texture to change. This can result in the formation of a new type of rock, such as from limestone to marble or from shale to schist.
When water freezes inside cracks in rocks, it expands and exerts pressure on the surrounding rock, causing it to fracture and break apart. Over time, this process, known as freeze-thaw weathering, can contribute to the formation of larger cracks and eventually lead to the breakdown of the rock into smaller pieces.
Chemical weathering is the type of weathering that involves a chemical change in some of the minerals in a rock. This process breaks down the rock into smaller pieces by altering its mineral composition through chemical reactions with substances like water, oxygen, or acids.
weathering occurs faster in warm and rainy climate. the rate of which soil forms depends on the climate and type of rock. so soil formation is faster when weathering is quicker too.
Hydration
Concentric weathering, also known as spheroidal weathering, is a type of physical weathering that occurs on rocks with uniform composition. It involves the gradual wearing away of outer layers of rock, resulting in the formation of onion-like layers or spheres on the surface of the rock. This type of weathering is commonly seen on boulders and large rock outcrops.
weathering and erosion
The type of rock formed when weathering, deposition, and cementation are all involved is sedimentary rock. Weathering breaks down rocks into sediments, which are then transported and deposited by water, wind, or ice. Cementation occurs when minerals precipitate and bind the sediments together to form solid rock.
Hydration weathering is a type of chemical weathering process where rocks absorb water and expand, leading to their breakdown and weakening. This process can cause minerals within the rock to dissolve or change in composition, ultimately breaking down the rock structure.
carbonation
Earthquakes mainly contribute to mechanical weathering by causing rocks to break apart due to the intense pressure and shaking. This can lead to the formation of smaller rock fragments and debris.
Chemical weathering
The type of weathering that does not alter the chemical composition of the rock is called physical weathering. The acid weathering usually alter the chemical composition of a rock.
Chemical weathering occurs when rock is broken down by chemical reactions as it absorbs water or other substances. These reactions can alter the minerals within the rock and cause it to physically weaken and disintegrate.
Chemical weathering is primarily responsible for the formation of most soil. This process involves the breakdown of rock and minerals through chemical reactions with water, air, and other substances, leading to the formation of soil particles. Over time, this weathering process helps to create fertile soil that supports plant growth.