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Drainage basins include the Antelope Valley watershed, the Mojave watershed, Mono Basin, the Owens River watershed, and the Amargosa River watershed. [3] There are 77 state-recognized alluvial groundwater basins and subbasins in the South Lahontan hydrologic region, underlying approximately 55 percent of the land area. [2]
The San Juan–Chama Project is a U.S. Bureau of Reclamation interbasin water transfer project located in the states of New Mexico and Colorado in the United States.The project consists of a series of tunnels and diversions that take water from the drainage basin of the San Juan River – a tributary of the Colorado River – to supplement water resources in the Rio Grande watershed.
The Mojave lies between the Sonoran (south) and the Great Basin (north). Here, soil is shallow, rocky, and dry. The average elevation is between 3,000–6,000 feet (910–1,830 m) above sea level. The Mojave has several mountain range boundaries, the Garlock and the San Andres. They are made up of the two largest faults in the state of California.
There are two water resource basin subdivisions of the Northern Mojave–Mono Lake subregion (HUC 1809). Northern Mojave–Mono Lake water resource subregion (HUC 1809) is one of 10 water resource subregions within the California water resource region and is one of 222 water resource subregions in the federally organized United States hydrologic unit system.
The Albuquerque Basin (or Middle Rio Grande Basin [1]) is a structural basin and ecoregion within the Rio Grande rift in central New Mexico. It contains the city of Albuquerque . Geologically, the Albuquerque Basin is a half-graben that slopes down towards the east to terminate on the Sandia and Manzano mountains. [ 2 ]
The Mojave River is the principal river reaching the Lake Mojave basin, [3] and the principal river of the Mojave Desert. [5] Presently, a number of springs on the western side of the Lake Mojave basin form small waterbodies. [5] The total watershed area is about 11,860 square kilometres (4,580 sq mi). [16]
The groundwater potential of the Santa Fe Group was recognized by Bryan Kirk in 1938, [18] and the Alamosa subbasin of the San Luis Valley, the central part of the Albuquerque Basin, and the southern Mesilla basin from Las Cruces to El Paso are now among the most productive groundwater reservoirs in the western United States. [19]
It formerly was the Mojave River's terminal lake, [5] and received about 1 millimetre per year (0.039 in/year) of sediment. [45] The Coyote Basin was not permanently coupled to the main lake body; its relatively large surface area and consequently high evaporation would have stabilized lake levels when it was connected to Lake Manix proper. [46]