Chemical weathering processes are particularly effective on limestone landscapes,forming

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Chemical weathering processes, particularly carbonation, are known to be highly effective on limestone landscapes, resulting in the formation of karst topography, such as sinkholes, caverns, and disappearing streams. Exfoliation domes and arch-like forms are caused by physical weathering processes such as thermal expansion and pressure release jointing, while hydrolysis plains are formed by chemical weathering of silicate rocks.

Chemical Weathering Processes Are Particularly Effective on Limestone Landscapes,forming