Final answer:
Around an actively pumped well in an unconfined aquifer, a cone of depression may develop in the water table.
Step-by-step explanation:
Around an actively pumped well in an unconfined aquifer, a cone of depression may develop in the water table.
A cone of depression occurs when the water table in the vicinity of a well drops, creating a cone-shaped area of lower water levels. This happens because the pumping of groundwater creates a temporary imbalance, causing nearby water levels to decrease.
The cone of depression represents the area where the water table is influenced by the pumping of the well. It is important to understand the concept of a cone of depression because it affects the availability of groundwater and can have significant impacts on ecosystems and water resources.