Underground water is more common in limestone areas than surface run off. Why?
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Solution: the main composition or content of limestone region is the calcium carbonate.
Moreover, calcium carbonate is soluble pure water but easily soluble in carbonated water.
At the surface run offs infiltration of the ground and solubility starts.
Moreover, formation of land forms and active precipitation is more common at his limestone region.
This is why underground water is more common than surface run offs which helps the processes to occur exclusively or inter-bedded.
Moreover, calcium carbonate is soluble pure water but easily soluble in carbonated water.
At the surface run offs infiltration of the ground and solubility starts.
Moreover, formation of land forms and active precipitation is more common at his limestone region.
This is why underground water is more common than surface run offs which helps the processes to occur exclusively or inter-bedded.
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