See more from this Division: Gulf Coast Association of Geological Societies
See more from this Session: Environmental Geology I and Hydrology
Abstract:
This study concluded that San Marcos Springs receives both local and regional flow with a greater component being derived from local sources during wet years and a greater component of regional flow during dry years. Three major fault blocks, part of the Balcones Fault Zone, influence groundwater flow from Bexar County eastward toward both San Marcos and Comal springs. Groundwater flows through the Artesian fault block and either discharges from Comal Springs or, depending upon stage, bypasses Comal Springs and discharges at San Marcos Springs. During dry periods, water levels in the Comal Springs and Hueco Springs fault blocks decline below Comal Springs orifice elevations, which precludes local recharge, although the orifices continue to discharge water from the Artesian fault block. During wet periods, San Marcos Springs is also recharged by water infiltrating from Cibolo Creek, the Guadalupe River, Dry Comal Creek, Sink Creek, and other streams, especially when a groundwater mound forms under Onion Creek. Despite the large volume of water that these streams carry at times, they contribute relatively small amounts to San Marcos springflow.
See more from this Division: Gulf Coast Association of Geological Societies
See more from this Session: Environmental Geology I and Hydrology