Scanned and georeferenced cross-sections from King ( 1937 ) shown in threedimensional space . The Marathon Aquifer outline is shown in red .
the Marathon Aquifer is mostly by the town of Marathon , though there are also a number of domestic wells present in the study area , most of which are in the vicinity of the town of Marathon .
In summary , there has been very little historical pumping from the Marathon Aquifer . Groundwater conditions are likely unaffected by pumping , with the possible exception of the area around the town of Marathon , where the majority of historical pumpage from the aquifer has occurred . The lowest year of aquifer recharge , 2011 , saw approximately 3,850 acre-feet added to the aquifer , while the highest recorded pumpage , in 2010 , only removed 450 acre-feet of water from it .
For a detailed description of the geology of the area , examples of the 3-D model of the aquifer , and a complete description of the methods used in the study , download the full report at www . twdb . texas . gov / groundwater / models / gam / mrtn / mrtn . asp . �
Scanned and georeferenced cross-sections from King ( 1937 ) shown in threedimensional space . The Marathon Aquifer outline is shown in red .
26 Cenizo Fall 2022