Flaking of rocks due to extrmees of temperature is called freeze-thaw erosion or exfoliation.
The flaking of rocks due to temperature extremes is called thermal stress weathering. This process occurs when rocks expand and contract due to heating and cooling, leading to the outer layers flaking off.
Signs of weathering include the gradual disintegration or wearing away of rocks and other materials on the Earth's surface due to exposure to environmental factors such as water, wind, and temperature changes. Common signs of weathering include cracks, fractures, flaking, and the rounding of sharp edges or corners on rocks and other structures. Weathering can also lead to the formation of soil and sediment.
Rocks expand due to heat and contract due to cold. Thus, due to unequal expansion and contraction ,the rocks tend to break and get weathered. Rocks expand due to heat and contract due to cold. Thus, due to unequal expansion and contraction ,the rocks tend to break and get weathered.
A continental climate features wide temperature extremes and grassy plains. This climate is characterized by hot summers and cold winters, with distinct seasonal variations in temperature. Grasslands are common in regions with this type of climate due to the lack of trees and shrubs.
The largest extremes in temperature are usually experienced in deserts, where the lack of vegetation and moisture allows for rapid heating during the day and quick cooling at night. Antarctica also experiences extreme temperature variations due to its ice-covered landscape and polar climate.
Without an atmosphere, there would be significant temperature extremes between day and night. During the day, the surface would become very hot due to direct sunlight, while at night, temperatures would drop rapidly without the atmosphere to trap heat. This difference is significant because the atmosphere helps regulate temperature by trapping heat and distributing it around the planet.
Weathering in geology means the chemical and mechanical breakdown of rocks that occurs due to the weakening of these rocks by changes in the environment, such as temperature.
Different erosional features can lead to layers of rock flaking off. In layered sedimentary rocks this is usually the case when some of the layers are less resistant against weathering (e.g. when the grains are cemented by carbonate which is dissolved by acid rain). One can often see that phenomenon on old sandstone buildings. Also igneous rocks show the effect of layers flaking off the surface. This may be related to thermal expansion and contraction working mostly on the outer part of large boulders. It might as well have something to do with the structure of the rock inherited from its crystallization and residual stresses and the depth that water can penetrate and weather the rock. Another answer: The flaking off in layers of rocks is called exfoliation. This usually occurs in deserts and is caused by changes in temperature.
The temperature in deserts 'swings' from one extreme to another. By day - the temperature rises to as much as 50C or more... at night the temperature can be as low as minus 40C ! This drastic fluctuation causes rocks expand and contract - which breaks them apart. The wind does the rest - 'sand blasting' the rocks until they're completely worn away.
Temperature can cause rocks to expand and contract, leading to stress fractures. This can weaken the rock structure over time, making it more susceptible to weathering and erosion. Additionally, extreme temperature variations can lead to physical weathering, such as thermal fracturing, where rocks break apart due to the stress caused by rapid heating and cooling.
Your cast iron seasoning may be flaking off due to a few reasons, such as not applying enough oil during seasoning, using high heat, or not properly cleaning and maintaining the pan. Re-seasoning the cast iron with multiple thin layers of oil can help prevent flaking in the future.
The chemical breakdown of rocks is called weathering. This process involves the physical and chemical breakdown of rocks into smaller pieces due to exposure to elements such as water, wind, and temperature changes.