San Bernardino Valley (Arizona)

For the valley in Southern California, see San Bernardino Valley.

The San Bernardino Valley of Arizona is a 35 mi (56 km) northeast-by-southwest trending valley in extreme southeast Cochise County, Arizona.^[1] The north end of the valley merges into the northwest-by-southeast trending San Simon Valley; both merge in western perimeter Hidaldgo County, New Mexico. The valley is an asymmetric graben.^[2]

San Bernardino Valley
Paramore Crater
San Bernardino Valley San Bernardino Valley in Arizona
Length	35 mi (56 km) NE x SW
Width	12 mi (19 km)
Geography
Country	United States
State	Arizona
Regions	Sonoran Desert Chihuahua Desert
Counties	Cochise County, Arizona Hidalgo County, New Mexico
Communities	Chiricahua, AZ Bernardino, AZ (historical site)
Borders on	List Chiricahua Mountains San Simon Valley Peloncillo Mountains Guadalupe Mountains San Bernardino National Wildlife Refuge Sierra del Tigre Perilla Mountains Pedrogosa Mountains
Coordinates	31°33′25″N 109°10′05″W

Valleys border all flanks of the Chiricahua Mountains massif (and some attached sub-ranges); The San Bernardino Valley borders the southeast of the Chiricahua Mountains; the San Simon Valley borders the northeast. San Bernardino Valley abuts the Peloncillo Mountains of New Mexico on the east, and the smaller adjoining range to its south, the Guadalupe Mountains. To the south, the valley borders Sonora, Mexico and the north regions of the Sierra del Tigre range, of Mexico. At the northern end of the Sierra del Tigre, the Rio San Bernardino joins the Bavispe River, then heads south to Mexico. To the northwest and west, the San Bernardino Valley abuts the Chiricahuas, Pedregosa, and Perilla Mountains.

At the very south of the valley, north of Douglas, Arizona–Agua Prieta, Mexico lies the San Bernardino National Wildlife Refuge. The refuge, grasslands, and wetlands are part of the south and southwest-flowing Yaqui River of Mexico that reaches the northeast region of the Gulf of California.

Geronimo–San Bernardino volcanic field

The San Bernardino Valley floor is covered by basaltic lava dating from 0.27 to 1.0 Ma^[3] (million years ago). The Geronimo–San Bernardino volcanic field is part of the larger Boot Heel volcanic field.

The field covers some 850 km² and consists of olivine basalt flows, tuff rings and maars with 130 identified volcanic vent areas and cinder cones.^[4]

References

1. "San Bernardino Valley Geography". azwater.gov. Retrieved October 17, 2010.
2. Wood, Charles A.; Jürgen Kienle (1993). Volcanoes of North America. Cambridge University Press. pp. 287–289. ISBN 0-521-43811-X.
3. M. J. Aldrich and A. W. Laughlin, 1981, Age and Location of Volcanic Centers < 3.0 M. Y. Old in Arizona, New Mexico and the Trans-Pecos Area of West Texas, LA-881 2-MAP, Revised
4. Evans, Stanley H. and W. P. Nash, Petrogenesis of xenolith-bearing basalts from southeastern Arizona, American Mineralogist, Volume 64, pp. 249–267, 1979

External links

• Media related to San Bernardino volcanic field at Wikimedia Commons
• The Yaqui River Drainage, Americas Heritage Waters, Northern Arizona University
• Cuenca Los Ojos Foundation
• Paramore Crater (coordinates), (Topoquest)