Rio San Jose Explained

Rio San Jose
Map:File:RioGrandeRiverMapNM.png
Subdivision Type1:Country
Subdivision Name1:United States
Subdivision Type2:State
Subdivision Name2:New Mexico
Subdivision Type4:County
Subdivision Name4:Cibola, Valencia, Bernalillo
Length:90miles
Source1:Zuni Mountains
Source1 Location:Bluewater Village, Valencia County
Source1 Coordinates:35.2872°N -107.9994°W
Source1 Elevation:6651feet
Mouth:Rio Puerco
Mouth Location:near Isleta Pueblo, Bernalillo County
Mouth Coordinates:34.8806°N -107.0278°W
Mouth Elevation:5102feet
Basin Size:2597sqmi[1]

The Rio San Jose is a 90miles tributary of the Rio Puerco in the U.S. state of New Mexico.

Course

The Rio San Jose's farthest tributary stream is Bluewater Creek; its headwaters are in the Zuni Mountains, near the continental divide in Cibola County, with about 400 feet of the course in McKinley County. Bluewater Creek is dammed to form Bluewater Lake, with a capacity of 43500acre feet.[2] The Rio San Jose proper starts at the confluence of Bluewater Creek and Mitchell Draw near Bluewater Village. Entering Valencia County, it flows southeast, through Grants, then turning east near McCartys, flowing through the Acoma Indian Reservation and Laguna Pueblo. The remains of an ancient dam constructed by the Laguna people sometime between 1370–1750 AD is situated within Laguna Pueblo.[3] Below Mesita the river turns southeast again, flowing through a narrow canyon before joining the Rio Puerco in Bernalillo County.

The entire course of the river below Bluewater Creek is roughly paralleled by the BNSF Railway tracks (formerly the Atlantic and Pacific Railroad, built around 1882, later absorbed into the AT&SF). Between Bluewater Village and Mesita the river valley provides the route for old U.S. Route 66 and I-40.

Hydrology

The water level and streamflow of the Rio San Jose has been measured at a number of sites in Cibola County, New Mexico. Stream gauges have been operated by the USGS near Laguna, Correo, and at Acoma Pueblo, near Grants.[4] [5] [6] The gauge at Acoma Pueblo has a record that commenced in 1937, and is the only one still active. It measures flow from a contributing area of 1170mi2, from a larger drainage basin of 2300mi2. The mean flow between 1937 and 2016 was, with the lowest daily flow recorded in July 2014 at .[4]

The highest river level recorded occurred in September 1963 with a height of through the gauge, giving a corresponding flow of, although this peak flow was affected by diversion or regulation.[4]

Since the 1870s the flow of the upper river has been substantially modified by demands for irrigation, groundwater abstraction and a dam on the Bluewater Creek. A report in 1982 showed that the natural flow was estimated to be between and, as opposed to the measured mean flow of .[7]

See also

Notes and References

  1. Web site: National Hydrography Dataset via National Map Viewer. U.S. Geological Survey. 2018-07-14.
  2. Web site: Bluewater Lake State Park. New Mexico State Parks. 2018-07-14.
  3. Web site: Identification and dating of indigenous water storage reservoirs along the Rio San José at Laguna Pueblo, western New Mexico, USA. Journal of Arid Environments. Gary Huckleberry, T.J. Ferguson, Tammy M. Rittenour, Chris Banet, and Shannon Mahan. U.S. Geologic Survey. 2016. 2018-07-14.
  4. Web site: USGS 08343500 RIO SAN JOSE – Summary Statistics. U.S. Geological Survey. National Water Information System. 10 July 2018.
  5. Web site: USGS 08350500 Rio San Jose near Laguna, NM . U.S. Geological Survey. National Water Information System. 10 July 2018.
  6. Web site: 08351500 Rio San Jose at Correo, NM. U.S. Geological Survey. National Water Information System. 10 July 2018.
  7. Web site: Estimated Natural Streamflow in the Rio San Jose Upstream from the Pueblos Of Acoma And Lacuna, New Mexico . U.S. Geological Survey. Risser . Dennis . 1982. 10 July 2018.