A rather simplified answer: Weathered rocks are broken down by ice, rain and wind, into smaller rocks, pebbles, sand, and silt. When the lighter sand and silt is carried by rivers, etc. and reaches the sea, it may form a layer on the sea bed. If the layer is placed under tremendous pressure, and is mainly of sand, sandstone is formed (over many eons). If mainly silt, slate is formed.
Sedimentary rock is formed when rocks are exposed to weathering and erosion. These processes break down existing rocks into smaller sediments, which are then transported, deposited, and compressed to form sedimentary rock over time. Examples include sandstone, limestone, and shale.
Chemical weathering
Hydration
Bauxite is an aluminum-rich sedimentary rock. It is the primary ore of aluminum and is formed through the weathering of aluminum-rich rocks in tropical environments.
Sedimentary rock forms from the layering of eroded rock material, which accumulates and undergoes compaction and cementation over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
The feature common to nearly every type of sedimentary rock is layering, known as stratification, which is formed by the accumulation and compaction of sediments over time. This layering provides information about the environment in which the rock was formed.
A Igneous B Sedimentary
Sedimentary rocks are formed from the weathering and erosion of pre-existing rocks. This process involves the breakdown of rocks into small particles that are then compacted and cemented together to form sedimentary rocks such as sandstone, shale, and limestone.
Sandstone is the sedimentary rock formed from weathered rock.
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.
Sedimentary rock is formed when rocks are exposed to weathering and erosion. These processes break down existing rocks into smaller sediments, which are then transported, deposited, and compressed to form sedimentary rock over time. Examples include sandstone, limestone, and shale.
It is possible, but not likely. It is more likely to undergo metamorphism, or be subjected to weathering and erosion, and end up as a different type of rock.
Chemical weathering
Hydration
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
mechanical weathering