Water School

Groundwater is water found beneath the Earth’s surface that gradually seeped down by saturating soil or rock. This water is stored in underground crevices and in the pores of rocks and other materials beneath the surface.

A water well is an artificial hole dug to access groundwater from aquifers.

Subsidence is a drop in the surface level of land. It sometimes occurs when groundwater is pumped from an aquifer. During this virtually irreversible process, cracks, fissures and sinkholes can appear in the ground.The southern area of the Brazos River basin has experienced a great deal of subsidence. To combat this problem, regulatory bodies known as subsidence districts were created by the State of Texas to begin lowering the use of groundwater and moving to a larger use of surface water in or...

Groundwater districts are organizations created by legislation or through the petition process to provide administration over the use of water pumped from a specific area.  These districts have limited power, primarily in the spacing of wells, education, and planning, prohibiting waste, and permitting well drilling.The Texas Commission on Environmental Quality has a myriad of information on groundwater supplies in Texas. The Texas Alliance of Groundwater Districts (TAGD) is an organiza...

A spring is a place where groundwater flows naturally from the Earth’s surface. There are two types: gravity springs and non-gravity springs. Gravity springs can be depression spring, surface springs, or artesian springs.  Depression springs: form when a water table intersects with the ground surface, and the water overflows. A water table is an underground boundary of soil saturation. These types of springs vary depending on the raising and lowering of the water table. ...

Major aquifers that lie within the basin or that are crossed by it include the Edwards BFZ, Seymour, Edwards-Trinity Plateau, Trinity, Ogallala, Carrizo-Wilcox and Gulf Coast.  For a full sized map, click here.