Groundwater is very important to the ongoing lives of most Americans. Groundwater grows our fields and gives us clean water to drink. Groundwater is the runoff from precipitation that has worked into the soil beneath the surface. Some groundwater that has saturated the ground can be seen in surface water as lakes. Most groundwater lies in the crust in porous rocks. The water either fills the voids between soil particles or fills the voids in rocks such as limestone.
Groundwater is very important because it grows many of the crops we eat and allows the rivers to remain full. There is an approaching problem in many states including Nebraska of the groundwater table slowly depleting. More and more wells are being drilled in Nebraska every year. When too much of the groundwater is pulled from the reservoirs the water level of the rivers begins to fall. This decline in the levels of the rivers will affect not only many important ecosystems but also decrease the supply of drinking water in many cities.
The red areas in the map below show where the groundwater has decreased in level in recent years.

This problem can be solved by limiting both the number of wells we drill and by monitoring their proximity to rivers. If they are too close they will decrease the river level so they must be drilled far enough away. Once the soil is no longer saturated there is nothing keeping surface water at the surface.




