Ground water in the San Juan Basin, New Mexico and Colorado
Lyford FP. 1979. Ground water in the San Juan Basin, New Mexico and Colorado. Water-Resources Investigations 79-73. USGS, Department of the Interior. Albuquerque, NM
Principal aquifers in the San Juan Basin of New Mexico and Colorado are the Entrada Sandstone, Westwater Canyon Member of the Morrison Formation, Gallup Sandstone of the Mesaverde Group, several sandstones in the Mesaverde Group above the Gallup (Dalton Sandstone Member of the Crevasse Canyon Formation, Point Lookout Sandstone, Menefee Formation, Cliff House Sandstone), and sandstones of Tertiary age. Most ground water flows from topographically high outcrop areas toward the San Juan River and Rio Grande valley. Much of the water may move through confining layers to other aquifers or to the land surface rather than discharging directly to the streams. Transmissivities of the sandstones range from 50 to 300 feet squared per day. Lowest dissolved-solids concentrations occur in or near outcrops of the sandstones and increase in the direction of ground-water flow. Concentrations range from less than 500 milligrams per liter to more than 30,000 milligrams per liter.
- Type
- Published Report
- Authors
- Lyford, Forest
- Date of Issue
- 1979-05
- Publisher
- USGS, Department of the Interior
- Units
- CHCU , WRD
- Keywords
- Aquifers, Clemson, Colorado, Flow, Geohydrology, Geology, Ground Water, Hydrogeology, New Mexico, Rio Grande Valley, San Juan Basin, San Juan River, transmissivity, Water Quality, Water Resources, WRBIB