A cliff on a coast will experience the most weathering due to wave action.
Marble is attacked by carbonic acid - carbon dioxide dissolved in water. The desert has little rainfall so chemical weathering occurs at a very slow rate.
All deserts are 'water thirsty.' That is why they are called deserts - they are arid regions that experience low rainfall. The Thar is no exception. If it received more rainfall it would cease to be a desert.
Clouds mean water, and deserts have virtually no water.
That would be the Arabian Desert.
That would depend upon which desert and your specific location in that desert.
Since it rarely rains in the Atacama, nearly all weathering would be physical weathering caused by the wind.
water and snow
Rock weathering is reduced in deserts because of the lack of moisture. Weathering processes such as chemical weathering rely on water to break down rocks, which is limited in desert environments. Additionally, the extreme temperature fluctuations in deserts can inhibit the expansion and contraction of rocks that would typically contribute to mechanical weathering.
Chemical weathering agents, such as acid rain, and biological weathering agents, such as plant roots, are less common in deserts due to the lack of moisture and vegetation in these arid environments. Wind and physical weathering, like abrasion and thermal stress, are more prevalent in desert weathering processes.
Chemical weathering agents like acid rain would be rare in the desert due to low moisture levels. Similarly, frost wedging, which requires water to freeze and expand, would also be less common in desert environments.
Depending on what type of desert, the atmosphere is usually dry, and sometimes windy. In a desert such as the Sahara, the weather is hot and dusty, although cooler at night. In a desert like Antarctica, the weather is extremely cold and windy.
Chemical weathering agents like acid rain and biological weathering agents like plant roots would be rare in deserts due to the lack of moisture needed for these processes to occur effectively. Instead, physical weathering agents like wind and temperature fluctuations are more common in desert environments.
Areas with high levels of precipitation and temperature fluctuations, such as tropical regions or coastal areas, typically experience more significant weathering due to the combination of mechanical and chemical processes. Additionally, areas with frequent freeze-thaw cycles or high levels of vegetation and organic material can also experience increased weathering.
Physical weathering from temperature changes is most common on the shorelines, because waves are able to take down rocks that have been weathers. They would be least noticeable inland, in desert areas with little forestation.
When Suzy sold seashells by the seashore, she was short-changing her sales potential. She should have sold seashells far from the seashore- somewhere that would show how special they really are. The seashore was littered with seaweed today.
Marble is attacked by carbonic acid - carbon dioxide dissolved in water. The desert has little rainfall so chemical weathering occurs at a very slow rate.
water and snow