Final answer:
If the rate of groundwater recharge exceeds the rate of withdrawal, regional water tables may be lowered. This statement is True.
Step-by-step explanation:
If the rate of groundwater recharge exceeds the rate of withdrawal, regional water tables may be lowered. This statement is True.
Groundwater recharge refers to the process of water percolating down into the ground and replenishing the underground aquifers. When the rate of recharge is greater than the rate of withdrawal (due to pumping of water from wells), the water tables can be maintained or even rise.
However, when the rate of withdrawal exceeds the rate of recharge, the water tables can be significantly lowered, leading to a decrease in available groundwater.