When a cone of depression forms around a well, the condition cannot be reversed. True False

**False**<br /><br />A cone of depression forms around a well when groundwater is pumped out faster than it can naturally recharge, causing the water table to lower in the vicinity of the well. However, this condition **can be reversed** if pumping is reduced or stopped, allowing the aquifer to recharge over time through natural processes like precipitation or infiltration from nearby water sources. The rate and extent of recovery depend on factors such as the aquifer's permeability, recharge rate, and overall water usage in the area.