Groundwater is the water found underground in the cracks and spaces within soil, sand and rock. It is stored in and moves gradually through geologic formations of soil, sand and rocks called aquifers.
Water is always on the move. From the time the earth was formed, it has been endlessly circulating through the hydrologic cycle. Groundwater is an important part of this continuous cycle as water evaporates, forms clouds, and returns to earth as precipitation and then the cycle starts again. Only a small percentage of the precipitated water (surface water) is able to peculate into the subsurface and contribute to a groundwater aquifer through the process of recharge.
Recharge rates will depend on various aspects such as climate, soil moisture, grain size, catchment topography ext. Once the water has joined the aquifer through recharge, it doesn’t stop there. The groundwater slowly moves through the spaces and cracks between the soil particles on its journey to lower elevations. This movement of water underground is called groundwater flow.
Eventually, after years of underground movement, the groundwater comes to a discharge area where it enters a lake or stream and becomes surface water. There, the water will once again be evaporated and begin the cycle again.