Final answer:
Groundwater is replenished by various sources such as seepage from surface water, deliberate pumping of surface water into the ground, irrigation, and underground wastewater treatment systems. Wetlands and aquifers act as recharge areas for groundwater. However, excessive pumping of groundwater can create a localized drop in the water table and result in a cone of depression, leading to a depletion of regional water resources.
Step-by-step explanation:
Groundwater is a significant, subsurface reservoir of fresh water. It exists in the pores between particles in dirt, sand, and gravel or in the fissures in rocks. Groundwater can flow slowly through these pores and fissures and eventually finds its way to a stream or lake where it becomes part of the surface water again. Many streams flow not because they are replenished from rainwater directly but because they receive a constant inflow from the groundwater below.
Other sources of groundwater include seepage from surface water (lakes, rivers, reservoirs, and swamps), surface water deliberately pumped into the ground, irrigation, and underground wastewater treatment systems (septic tanks). Recharge areas are locations where surface water infiltrates the ground rather than running into rivers or evaporating. Wetlands, for example, are excellent recharge areas. A large area of sub-surface, porous rock that holds water is an aquifer. Aquifers are commonly drilled, and wells installed, to provide water for agriculture and personal use.