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Lots of rain, wind, freeze/thaw cycles. Hot, humid climates with high rainfall promote chemical weathering.
Hot, wet, tropical climates are most conducive to chemical weathering.
Chemical weathering occurs more rapidly in a hot, wet climate because chemical reactions speed up with increased temperature.
There are two types of weathering that occur: chemical weathering and physical weathering. One example of physical weathering is crushing a rock with a hammer. An example of chemical weathering is acid rain where the material is chemically broken down because of the rain's acidity.
rain,wind,freezing..
Physical weathering, such as cracks, creates more surface area for chemical weathering to occur on.
Wet. Hot and wet climates allow for the fastest weathering.
Lots of rain, wind, freeze/thaw cycles. Hot, humid climates with high rainfall promote chemical weathering.
Hot, wet, tropical climates are most conducive to chemical weathering.
There are two types of weathering: chemical and physical. Chemical weathering is said to occur when the chemical compounds of rocks are changed. Physical weathering happens due to wind, rain, or other natural occurrences.
Chemical weathering occurs more rapidly in a hot, wet climate because chemical reactions speed up with increased temperature.
There are two types of weathering that occur: chemical weathering and physical weathering. One example of physical weathering is crushing a rock with a hammer. An example of chemical weathering is acid rain where the material is chemically broken down because of the rain's acidity.
The process that creates soil from bare rock is called"weathering". The chemical and physical processes of [weathering] transform igneous rock.
rain,wind,freezing..
Weathering and erosion occur all the time even when mountains are forming
mechanical weathering
In the Stratosphere