This article focus to Discuss Effects of Groundwater Flow. The actual dissolution of calcite through limestone by slightly acidic ground‐water ends up with the gradual widening connected with cracks and joints that will ultimately develop into a number of openings, or caves. Most caves develop below the river table. After the caves are elevated above the river table or when the river table drops, the water drains out as well as the caves become filled with air.
Discuss Effects of Groundwater Flow
