San Ysidro Mountains
Otay Mountains
The Cerro San Isidro (top) and Otay Mountain (bottom)
Highest point
Elevation3,568 ft (1,088 m) NAVD 88[1]
Geography
San Ysidro Mountains is located in California
San Ysidro Mountains
location of San Ysidro Mountains in California[2]
CountryUnited States and Mexico
StateCalifornia and Baja California
DistrictSan Diego County and Tijuana Municipality
Range coordinates32°35′48.212″N 116°49′24.075″W / 32.59672556°N 116.82335417°W / 32.59672556; -116.82335417
Parent rangePeninsular Ranges
Topo mapUSGS Otay Mountain
BiomeCalifornia chaparral and woodlands

The San Ysidro Mountains are a mountain range in southern San Diego County, California[2] and Baja California, Mexico. The mountains are a rugged coastal foothill range of the Peninsular Ranges system. Major peaks include the highest summit of the range, Otay Mountain, and the Cerro San Isidro which forms the southern extrusion of the range on the Mexican side of the border. The majority of the range is within the Otay Mountain Wilderness Area, in the United States.

Geography

The San Ysidro Mountains are towards the top of this image. On the upper center of the image, the neighborhood of Valle Imperial can be seen reaching into the Cerro San Isidro.

Lying only 13 to 21 miles (21 to 34 km) inland from the Pacific Ocean, this mountain range rises out of the coastal plain of San Diego and Tijuana until it reaches a maximum height of 3,568 feet (1,088 m) on the summit of Otay Mountain. On the western side of the mountain lies Lower Otay Lake and Otay Mesa, with the Richard J. Donovan Correctional Facility and other detention centers and law enforcement properties lying on the southwest slope of the mountain.[3] On the eastern flank, Mine Canyon and Marron Valley separate the San Ysidro Mountains from Tecate Peak (Kuuchamaa).[4]

Cerro San Isidro

The Cerro San Isidro, located in Tijuana, is separated from the rest of the range by the border fence and the Rio Alamar, and forms the southern portion of the mountains. The summit of the Cerro San Isidro reaches approximately 2,750 feet (840 m), and supports many of the same endemic and rare plants found on Otay Mountain.[5] A colonia of Tijuana, Valle Imperial, stretches across the western slope of the mountain.[6]

On December 31, 2014, a rare snowfall event blanketed the Cerro San Isidro after low temperatures of 4 °C (39 °F).[6]

Ecology

The native vegetation of the San Ysidro Mountains represents the coastal sage scrub of the California coastal sage and chaparral ecoregion (western faces); and plants of the California montane chaparral and woodlands ecoregion (inland). The San Ysidro Mountains are one of the few locations the rare Tecate Cypress (Cupressus forbesii) is found. This tree was once abundant in the higher elevations of the range as well as in its canyons. The San Ysidro Mountains were deforested of living foliage by wildfires in 2003 and 2007. Cupressus forbesii is a fire ecology dependent species, and there has been some evidence of regrowth starting.

See also

References

  1. "Otay". NGS Data Sheet. National Geodetic Survey, National Oceanic and Atmospheric Administration, United States Department of Commerce. Retrieved 2021-09-19.
  2. 1 2 "San Ysidro Mountains". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2009-05-04.
  3. "South County Segment - San Diego County MSCP Subarea Plan" (PDF). San Diego County.
  4. Todd, Victoria R.; Lee, Gregory K.; Oliver, Howard W.; Causey, J. Douglas; Schmauch, Steven W. (1988). "Mineral Resources of the Southern Otay Mountain and Western Otay Mountain Wilderness Study Areas, San Diego County, California" (PDF). U.S. Geological Survey Bulletin. 1711 via USGS.
  5. Clark, Kevin B.; Dodero, Mark (January 2009). "The Threatened Biological Resources of Jesus Maria Mesa, Mexico". California Native Plant Society Conservation Conference via ResearchGate.
  6. 1 2 "Sorprende nevada en Este de Tij". Noticias de Tijuana | EL IMPARCIAL (in European Spanish). 1 January 2015. Retrieved 5 September 2022.
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