somebody answer this question please.
Mechanical weathering, also known as physical weathering, only affects the size and shape of the rock without changing its mineral composition. This can be caused by processes such as freeze-thaw cycles, root wedging, and salt crystal growth.
Physical weathering affects the size of a sample by breaking down rocks into smaller pieces through processes like frost wedging, exfoliation, and abrasion. These physical processes can reduce the size of the sample by breaking it into smaller fragments.
Climate affects weathering by influencing the rate and type of weathering processes that occur. In regions with high temperatures and abundant rainfall, weathering processes such as chemical weathering are more common due to increased moisture and chemical reactions. Conversely, in cold and dry climates, physical weathering processes like freeze-thaw can be more prevalent. Overall, climate plays a significant role in shaping the landscape through weathering processes over time.
Physical weathering contributes to the breakdown of rocks into smaller fragments, which eventually accumulate and form sand. These sand grains are then cemented together over time to create sandstone. Examples of physical weathering processes that contribute to sandstone formation include abrasion from wind or water, freeze-thaw cycles, and thermal expansion and contraction.
Some rocks commonly formed by weathering include sandstone, shale, and limestone. Sandstone is formed from the accumulation of sand grains cemented together, shale from the compaction of mud and clay, and limestone from the precipitation of calcium carbonate. These rocks can be broken down and altered by various weathering processes such as mechanical, chemical, and biological weathering.
because of people
Some factors that affect the rate of weathering are the type of rock, the altitude and the climate.
Sandstone is the sedimentary rock formed from weathered rock.
i think sandstone
Mechanical weathering, also known as physical weathering, only affects the size and shape of the rock without changing its mineral composition. This can be caused by processes such as freeze-thaw cycles, root wedging, and salt crystal growth.
The most important factors that determine the rate at which weathering occurs are the type of rock and the climate. Rainfall affects the rate of weathering.
Physical weathering affects the size of a sample by breaking down rocks into smaller pieces through processes like frost wedging, exfoliation, and abrasion. These physical processes can reduce the size of the sample by breaking it into smaller fragments.
Arkose is a type of sandstone that contains abundant feldspar, typically in the form of pink or red grains. Feldspar-rich sandstones are formed from the weathering and erosion of granitic rocks, which are rich in feldspar minerals.
Climate affects weathering by influencing the rate and type of weathering processes that occur. In regions with high temperatures and abundant rainfall, weathering processes such as chemical weathering are more common due to increased moisture and chemical reactions. Conversely, in cold and dry climates, physical weathering processes like freeze-thaw can be more prevalent. Overall, climate plays a significant role in shaping the landscape through weathering processes over time.
there is the 3 type of sandstone quatrz-arenite arkose graywacke
Physical weathering contributes to the breakdown of rocks into smaller fragments, which eventually accumulate and form sand. These sand grains are then cemented together over time to create sandstone. Examples of physical weathering processes that contribute to sandstone formation include abrasion from wind or water, freeze-thaw cycles, and thermal expansion and contraction.
Sandstone.