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# Closing forest
# Closing forest
Rock that composed high CaCO3 is dissolvable. Higher CaCO3 composition, karst morphology will develop. The compaction of rock determines stability of karst morphology after dissolution. If soft rock, then every visible karst that formed like karen and hill will be fast to vanish because of dissolution process itself or erosion and mass flow, therefore karst visibility cant developed. Thickness determines the form of vertical water circulation more, without thick layer, vertical water circulation that is requirements of karstification can ongoing. Without vertical circulation, process that ongoing is lateral flow like on surface rivers and close basins can’t form. Rock fissures are way to enter water formed vertical drainage and developing Sub-surface River and concentrate dissolution
Rock that composed high CaCO3 is dissolvable. Higher CaCO3 composition, karst morphology will develop. The compaction of rock determines stability of karst morphology after dissolution. If soft rock, then every visible karst that formed like karen and hill will be fast to vanish because of dissolution process itself or erosion and mass flow, therefore karst visibility cant developed. Thickness determines the form of vertical water circulation more, without thick layer, vertical water circulation that is requirements of karstification can ongoing. Without vertical circulation, process that ongoing is [[lateral]] flow like on surface rivers and close basins can’t form. Rock fissures are way to enter water formed vertical drainage and developing Sub-surface River and concentrate dissolution
Fall of rain is main dissolution media in karstification process. Higher fall of rain, higher dissolution media, until level of dissolution that occur in limestone becomes higher. Elevation of limestone that exposed in surface determines vertical circulation/drainage.
Fall of rain is main dissolution media in karstification process. Higher fall of rain, higher dissolution media, until level of dissolution that occur in limestone becomes higher. Elevation of limestone that exposed in surface determines vertical circulation/drainage.