Migration of Recharge Water Downgradient from the Santa Catalina Mountains into the Tucson Basin Aquifer
Aquifers in the arid alluvial basins of the southwestern U.S. are recharged predominantly by infiltration from streams within the basins and by water entering along the margins of the basins from surrounding mountains (mountain -front recharge). The Tucson Basin of Southeastern Arizona is such a bas...
| Main Author: | |
|---|---|
| Other Authors: | |
| Language: | en_US |
| Published: |
The University of Arizona.
1996
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10150/249235 |