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The Edwards Aquifer is the primary water source for much of southern central Texas. [1] Burrell Day and Joel McDaniel owned a 350-acre ranch in Van Ormy, Bexar County. [2] Under the Edwards Aquifer Authority Act (EAAA), landowners who had historically used Edwards Aquifer groundwater for irrigation purposes were assured of a minimum permit amount of 2 acre-feet of production per year per acre ...
Located in South Central Texas, the Edwards Aquifer encompasses an area of approximately 4,350 square miles (11,300 km 2) that extends into parts of 11 counties. [3] The aquifer's boundaries begin at the groundwater divide in Kinney County, East of Brackettville, and extend Eastward through the San Antonio area and then Northeast where the aquifer boundary ends at the Leon River in Bell County ...
TxGIO provides a central access point for Texas Natural Resources data, census data, digital and paper maps, and information about datasets collected by state agencies and other organizations. It publishes historical and current aerial photography and printed topographic maps from the United States Geological Survey as part of its public domain ...
In Texas, there are 98 of these districts, covering nearly 70% of the state, according to the Texas Water Development Board. The Upper Trinity Groundwater Conservation District has the following ...
This is an accepted version of this page This is the latest accepted revision, reviewed on 29 January 2025. Water located beneath the ground surface An illustration showing groundwater in aquifers (in blue) (1, 5 and 6) below the water table (4), and three different wells (7, 8 and 9) dug to reach it. Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in ...
Raymond Straub, a hydrogeologist who owns a Texas groundwater services firm, testified at an October EPA hearing that he was concerned Occidental did not devote enough attention to the unplugged ...
The maps build on a new but growing body of research. In 2020, ... Explore current groundwater conditions in this interactive map: Patterns emerged. Many of the communities most exposed to ...
Groundwater is water that is found underground in cracks and spaces in the soil, sand and rocks. Where water has filled these spaces is the phreatic (also called) saturated zone. Groundwater is stored in and moves slowly (compared to surface runoff in temperate conditions and watercourses) through layers or zones of soil, sand and rocks: aquifers.