it expands n cracks n crack goes bigger n it falls of n shizzle
Another example of freeze-thaw weathering is when water seeps into cracks in rocks or pavement, freezes overnight, expands, and then thaws during the day. This repeated process causes the rock or pavement to crack and break apart over time.
Freeze-thaw weathering is a type of physical weathering caused by repeated cycles of freezing and thawing of water in cracks and pores of rocks. When water freezes, it expands, creating internal pressure that can crack the rock. Over time, this process can break down rocks into smaller pieces.
The process of which freeze-thaw or physical weathering takes place is rather simple. Firstly, water would get into cracks on a rock or hard material, and overnight, it would freeze. Secondly, because when water freezes, it expands, it therefore forces itself further into the rock; the crack is made larger. Lastly, this would created more space inside the rock, for more water to end up inside, and join in with the freeze-thaw, until finally, the rock would break.
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.
physical weathering
Freeze - Thaw weathering Onion skin weathering Erosion from rain water
Natural agents of physical weathering: Rain, sand (driven by the wind), sunlight, the freeze/thaw cycle. Man-made agents of physical weathering: Acid rain.
Another example of freeze-thaw weathering is when water seeps into cracks in rocks or pavement, freezes overnight, expands, and then thaws during the day. This repeated process causes the rock or pavement to crack and break apart over time.
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 type of physical weathering caused by repeated cycles of freezing and thawing of water in cracks and pores of rocks. When water freezes, it expands, creating internal pressure that can crack the rock. Over time, this process can break down rocks into smaller pieces.
The process of which freeze-thaw or physical weathering takes place is rather simple. Firstly, water would get into cracks on a rock or hard material, and overnight, it would freeze. Secondly, because when water freezes, it expands, it therefore forces itself further into the rock; the crack is made larger. Lastly, this would created more space inside the rock, for more water to end up inside, and join in with the freeze-thaw, until finally, the rock would break.
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
Mechanical weathering.
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.