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Magnetotelluric data in the middle Rio Grande basin, Albuquerque volcanoes, New Mexico

Open-File Report 2002-44

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Abstract

The population in the Albuquerque-Santa Fe region of New Mexico is rapidly growing. The Santa Fe Group aquifer in the Middle Rio Grande Basin is the main source of municipal water for the greater Albuquerque metropolitan area. The capacity of this aquifer is more limited than previously thought (Thorn et al., 1993). The Middle Rio Grande Basin, as defined hydrologically and used here, is the area within the Rio Grande Valley extending from Cochiti Dam downstream to the community of San Acacia (Figure 1). Because approximately 600,000 people (40 percent of the population of New Mexico) live in the study area (Bartolino, 1999), water shortfalls could have serious consequences. Future growth and land management in the region depends on accurate assessment and protection of the region’s groundwater resources. An important issue in defining the ground water resources is a better understanding of the hydrogeology of the Santa Fe Group and the other sedimentary deposits that fill the Rio Grande rift.

Additional publication details

Publication type:
Report
Publication Subtype:
USGS Numbered Series
Title:
Magnetotelluric data in the middle Rio Grande basin, Albuquerque volcanoes, New Mexico
Series title:
Open-File Report
Series number:
2002-44
Year Published:
2002
Language:
English
Publisher:
U.S. Geological Survey
Publisher location:
Denver, CO
Description:
90 p.
Country:
United States
State:
New Mexico