No. Chemical weathering is to do with acidic rain. This is a type of physical weathering, where it isn't the rainwater's ph, but the fact it freezes in cracks, expands, and prises the rock apart(creating a broken skyline or a scree slope). It occurs in damp areas where water is sometimes, not always below freezing.
Freeze-thaw weathering is a gradual process that can occur over many years or even centuries, depending on the frequency of freeze-thaw cycles and the type of rock or material being weathered. Factors such as climate, temperature fluctuations, and the composition of the rock can also influence the speed at which freeze-thaw weathering occurs.
Freeze-thaw refers to the process of water freezing and then thawing, which can cause physical weathering of rocks and damage to infrastructure due to the expansion and contraction of water. It is a common phenomenon in regions with fluctuating temperatures, leading to the formation of ice wedging and frost heaving.
Chalk is primarily affected by physical weathering processes like freeze-thaw cycles and abrasion by wind or water. Chemical weathering can also occur, particularly from exposure to acidic rain or groundwater which can dissolve the calcium carbonate in chalk. Over time, these processes can cause chalk to erode and crumble.
Mechanical weathering involves physical processes that break down rocks into smaller pieces, such as freeze-thaw cycles or root growth. Chemical weathering involves chemical reactions that alter the composition of rocks, like oxidation or dissolution. Overall, mechanical weathering physically breaks down rocks, while chemical weathering changes their chemical makeup.
Glacier action involves primarily mechanical weathering, as the movement of glaciers causes rocks to break apart through the physical forces of compression and abrasion. However, chemical weathering can also occur in glacial environments through processes like freeze-thaw cycles and the introduction of chemical substances from the ice.
Freeze/thaw cycles are an example of mechanical weathering of rock.
# Onion skin # Chemical # Abrasion # Mechanical # Freeze/thaw
physical weathering
Chemical(acid in rainwater dissolving limestone), biological (work of animals and plants) and physical (freeze thaw)
1) Physical weathering can be split into 2 subgroups-Freeze Thaw and Onion Skin! 2) Chemical Weathering! 3) Biological Weathering!
Freeze-thaw weathering is a gradual process that can occur over many years or even centuries, depending on the frequency of freeze-thaw cycles and the type of rock or material being weathered. Factors such as climate, temperature fluctuations, and the composition of the rock can also influence the speed at which freeze-thaw weathering occurs.
freeze and thaw, exfoliation and abrasion
Freeze - Thaw weathering Onion skin weathering Erosion from rain water
freeze-thaw weathering and onion skin weathering.
Freeze-thaw refers to the process of water freezing and then thawing, which can cause physical weathering of rocks and damage to infrastructure due to the expansion and contraction of water. It is a common phenomenon in regions with fluctuating temperatures, leading to the formation of ice wedging and frost heaving.
Chalk is primarily affected by physical weathering processes like freeze-thaw cycles and abrasion by wind or water. Chemical weathering can also occur, particularly from exposure to acidic rain or groundwater which can dissolve the calcium carbonate in chalk. Over time, these processes can cause chalk to erode and crumble.
Mechanical weathering involves physical processes that break down rocks into smaller pieces, such as freeze-thaw cycles or root growth. Chemical weathering involves chemical reactions that alter the composition of rocks, like oxidation or dissolution. Overall, mechanical weathering physically breaks down rocks, while chemical weathering changes their chemical makeup.