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Tecolote Canyon’s history writ in stone and sediment
A pleasant walk along the southern section
Area of the trail with views of the canyon
Tecolote Canyon, featured on area maps for almost 200 years, is designated a natural park 6 miles in length, .25 to .5-mile wide, with a 2-mile tributary totaling just over 900 acres. Elevations range from sea level at the canyon mouth to 320 feet at the head of Tecolote Canyon. The canyon rim is between 315 and 400 feet above sea level.
Trees along the trail
The geology of the park consists primarily of marine and nonmarine sedimentary rocks of the Scripps and Friars Formations of the Eocene Age (45–50 mya). These rocks make up the canyon walls, with Quaternary (1.8 mya) sedimentary rocks capping the mesas. The exception is at the canyon mouth where the northern wall into Bay Park consists of sediments of the Bay Point Formation of the Quaternary age (200,000 years). The Tecolote recreation center sits on marine sandstone of the San Diego Formation of Pliocene age (2–3 mya). The canyon floor consists of Holocene (recent) alluvium and slope wash.
Four faults have been mapped in the park, all located near the mouth. Behind the fence at center field of the upper baseball field, the Rose Canyon Fault can be seen where the margins show 50 mya Eocene sandstone of the Scripps Formation against red stippled Pleistocene conglomerate of only a half-million years. The Rose Canyon Fault parallels the San Andreas fault, extending north through La Jolla Shores.
Once past the baseball fields and nature center, follow the access road or trails that parallel first the water channel, then in the direction of the power lines to the end of the golf course, and then east to Genesee Ave. and back. The 4-mile walk turnaround point is at the peak of the hill under the power lines that overlooks the golf course. The longer hike follows the trail closest to the golf course. At the end of the course, turn east to Genesee Ave. and then head back.
Tecolote Canyon trail
Along the trail look for evidence of owls that the canyon is named for or other birds that include California thrashers, house wrens, hawks, towhees, and ravens. The walk along the trails and/or access road is a combination of good examples of coastal sage scrub, chaparral, and riparian habitats mixed with erosion and power lines.
Tecolote Creek north of the golf course can run to a depth of 6–8 feet during the rainy season. In the summertime, the creek is normally dry, except for runoff from the course greens. The creek empties into Mission Bay at the Pacific Passage side of Fiesta Island. The creek also contributes to the groundwater table in the lower end of the canyon.
In 1957, the city government planned to use Tecolote Canyon as a sanitary landfill where cattle had grazed until 1953. This and other development plans were abandoned due to protests from residents of Linda Vista and Clairemont leading to the Park Procedural Ordinance adopted by the San Diego City Council in 1969. The Tecolote Canyon Park District was initiated by the council in January 1971, then adopted in July 1974, both by a unanimous vote. After the land acquisition was completed, the dedication ceremony was held on April 1, 1978.
Distance from downtown San Diego: Approximately 6 miles. From I-5, take exit 21 for Sea World Dr./Tecolote Rd. Turn right onto Tecolote Rd. and within a mile park at the nature center. The Tecolote Nature Center when open has facilities and water.
Hiking length: The hike described here is 4 miles, though it can be extended to a 6.5-mike hike if the trail is followed close to the intersection of Genesee Ave. and Marlesta Dr. and back.
Difficulty: Easy to moderate, depending on distance walked, with an elevation gain near 400 feet.
Here's something you might be interested in.
Tecolote Canyon’s history writ in stone and sediment
A pleasant walk along the southern section
Tecolote Canyon’s history writ in stone and sediment
A pleasant walk along the southern section
Area of the trail with views of the canyon
Tecolote Canyon, featured on area maps for almost 200 years, is designated a natural park 6 miles in length, .25 to .5-mile wide, with a 2-mile tributary totaling just over 900 acres. Elevations range from sea level at the canyon mouth to 320 feet at the head of Tecolote Canyon. The canyon rim is between 315 and 400 feet above sea level.
Trees along the trail
The geology of the park consists primarily of marine and nonmarine sedimentary rocks of the Scripps and Friars Formations of the Eocene Age (45–50 mya). These rocks make up the canyon walls, with Quaternary (1.8 mya) sedimentary rocks capping the mesas. The exception is at the canyon mouth where the northern wall into Bay Park consists of sediments of the Bay Point Formation of the Quaternary age (200,000 years). The Tecolote recreation center sits on marine sandstone of the San Diego Formation of Pliocene age (2–3 mya). The canyon floor consists of Holocene (recent) alluvium and slope wash.
Four faults have been mapped in the park, all located near the mouth. Behind the fence at center field of the upper baseball field, the Rose Canyon Fault can be seen where the margins show 50 mya Eocene sandstone of the Scripps Formation against red stippled Pleistocene conglomerate of only a half-million years. The Rose Canyon Fault parallels the San Andreas fault, extending north through La Jolla Shores.
Once past the baseball fields and nature center, follow the access road or trails that parallel first the water channel, then in the direction of the power lines to the end of the golf course, and then east to Genesee Ave. and back. The 4-mile walk turnaround point is at the peak of the hill under the power lines that overlooks the golf course. The longer hike follows the trail closest to the golf course. At the end of the course, turn east to Genesee Ave. and then head back.
Tecolote Canyon trail
Along the trail look for evidence of owls that the canyon is named for or other birds that include California thrashers, house wrens, hawks, towhees, and ravens. The walk along the trails and/or access road is a combination of good examples of coastal sage scrub, chaparral, and riparian habitats mixed with erosion and power lines.
Tecolote Creek north of the golf course can run to a depth of 6–8 feet during the rainy season. In the summertime, the creek is normally dry, except for runoff from the course greens. The creek empties into Mission Bay at the Pacific Passage side of Fiesta Island. The creek also contributes to the groundwater table in the lower end of the canyon.
In 1957, the city government planned to use Tecolote Canyon as a sanitary landfill where cattle had grazed until 1953. This and other development plans were abandoned due to protests from residents of Linda Vista and Clairemont leading to the Park Procedural Ordinance adopted by the San Diego City Council in 1969. The Tecolote Canyon Park District was initiated by the council in January 1971, then adopted in July 1974, both by a unanimous vote. After the land acquisition was completed, the dedication ceremony was held on April 1, 1978.
Distance from downtown San Diego: Approximately 6 miles. From I-5, take exit 21 for Sea World Dr./Tecolote Rd. Turn right onto Tecolote Rd. and within a mile park at the nature center. The Tecolote Nature Center when open has facilities and water.
Hiking length: The hike described here is 4 miles, though it can be extended to a 6.5-mike hike if the trail is followed close to the intersection of Genesee Ave. and Marlesta Dr. and back.
Difficulty: Easy to moderate, depending on distance walked, with an elevation gain near 400 feet.
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