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Location: 22 km N from Goliad, Texas, United States
500 North Shoreline Ste. 800NCorpus ChristiTexas, United States78401
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Uranium mineralization at the Goliad Project Area is typical of Texas roll-front sandstone deposits. All mineralization at the Goliad Project Area occurs in the Goliad Formation. The Goliad Formation occurs at surface on the Goliad Project Area. The mineralized units are sandstones within the Goliad Formation and are designated by UEC as the A through D sands from younger (upper) to older (lower), respectively. The sand units are generally fine to medium-grained sands with silt and varying amounts of secondary calcite. The sand units vary in color depending upon the degree of oxidation-reduction and could be from light brown-tan to gray. The sand units are generally separated from each other by silty clay or clayey silts that serve as confining units between the sand units. The four sandstone units (A-D) designated as containing uranium mineralization at the site are all considered to be a part of the Gulf Coast Aquifer on a regional basis. At the Goliad Project Area, each unit is a hydrogeologic unit with similar but variable characteristics. Groundwater from sands of the Goliad Formation is used for water supplies over much of the northern portion of Goliad County. The Goliad structures include two faults that intersect and offset the mineralized units. These faults are normal faults, with one downthrown toward the coast and one downthrown toward the northwest. The fault throws range from about 40 to 80 feet. The Goliad sand is one of the principal water-bearing formations in South Texas and can yield moderate to large quantities of water. All of the project areas included in this Goliad Project Area target the Goliad Formation, which is a proven aquifer with characteristics favorable to ISR.
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