STRATIGRAPHIC EVALUATION OF TRINITY AQUIFERS IN HAYS AND WESTERN TRAVIS COUNTY AND IMPLICATIONS FOR GROUNDWATER AVAILABILITY
Results suggest that there are stratigraphic variations in the Middle and Lower Trinity units that may influence groundwater availability. From stratigraphic top to bottom, the Upper Glen Rose is a regionally consistent carbonate interval. The Middle Trinity Aquifer is composed of the Lower Glen Rose, Hensel and Cow Creek limestone. The discontinuous nature of the biostrome/reef intervals in the Lower Glen Rose appears to correlate to poor water quality and poor yield where the reef is absent. The Hensel, which transitions from a predominantely clastic and water bearing interval in the updip areas, to a thinner silty, dolomitic aquitard internval downdip. The underlying Cow Creek indicats a facies transition from an updip grainstone to dolomite in the downdip areas with higher yields. The underlying Hammett is a regionally consistent clay and aquitard unit for the Middle Trinity.
In addition to high levels of pumping, groundwater availability appears to be influenced by facies changes within the Middle Trinity units of the study area. Understanding the detailed straigraphy will provide insights into these important groundwater resources.