Los Trancos Creek | |
---|---|
Etymology | Spanish language |
Location | |
Country | United States |
State | California |
Region | Northwestern Santa Clara County and southeastern San Mateo County |
City | Portola Valley, Menlo Park, Stanford University |
Physical characteristics | |
Source | |
• location | Los Trancos Open Space Preserve on the northwest slope of Monte Bello Ridge |
• coordinates | 37°19′41″N122°10′35″W / 37.32806°N 122.17639°W [1] |
• elevation | 2,080 ft (630 m) |
Mouth | San Francisquito Creek |
• location | West edge of Stanford University below Interstate 280 |
• coordinates | 37°24′50″N122°11′30″W / 37.41389°N 122.19167°W [1] |
• elevation | 164 ft (50 m) |
Basin features | |
Tributaries | |
• left | Bovet Creek |
• right | Buckeye Creek (East Fork Los Trancos Creek), Felt Creek |
Los Trancos Creek (meaning "barriers" or "cattle guards" from the Spanish "Las Trancas" [2] ) is a creek that flows northerly from Monte Bello Ridge on the northeast slope of the Santa Cruz Mountains to its confluence with San Francisquito Creek at Stanford University in California, United States. The creek forms the boundary between northwestern Santa Clara County and southeastern San Mateo County.
High winter flows in Los Trancos Creek are diverted by Stanford's Lagunitas Diversion Dam just downstream from Rossotti's to Felt Lake. The lake is actually a reservoir that lies west of Interstate 280 and bounded by Alpine Road and the Pearson Arastradero Preserve on Arastradero Road. Felt Lake was constructed in 1876 by gold miner and lumber dealer Job Johnston Felt, who bought 700 acres in northern Santa Clara County to farm. It was his dream to build two water companies, San Francisquito and Los Trancos. Felt built the original diversion from Los Trancos Creek to Felt Lake. By the mid-1880s, and facing opposition to his plans, the elderly Felt abandoned the water company idea and sold the farm to Timothy Paige, who quickly sold it to Leland Stanford Sr. in 1887. The university later added a larger dam to hold irrigation water for the growing campus.? [3]
Los Trancos Creek drains an area of about 7 square miles (18 km2) and consists of about 6.6 miles (10.6 km) of channel. [4] Its headwaters are protected by the Los Trancos Open Space Preserve just northwest of Page Mill Road.
Los Trancos Creek has several minor tributaries. Named tributaries are Bovet Creek, Buckeye Creek, and Felt Creek. Bovet Creek begins in Coal Mine Ridge Open Space Preserve of Portola Valley Ranch, and is named after the local prominent ranch owner, Antoine Francis Bovet, who died in 1973. [5] Bovet Creek flows down along Valley Oaks Street in Buckeye Creek is a small tributary that enters from the east with origins in Palo Alto Foohills Park, including Boronda Reservoir. Felt Creek is another small ephemeral tributary which begins in the Pearson-Arastradero Preserve, then passes north under Arastradero Road where it was dammed to create Felt Lake. The Felt Lake Diversion ditch begins at the intersection of Arastradero and Alpine Roads and diverts high winter Los Trancos Creek flows to join Felt Creek before the latter enters Felt Lake. Below the reservoir, Felt Creek rejoins Los Trancos Creek just north of Interstate 280. [6] Of interest, Felt Creek may have historically joined Los Trancos Creek just north of Arastradero Road on the 1876 Thompson & West map of Santa Clara County. [7]
The next watershed to the west is Corte Madera Creek, another tributary of San Francisquito Creek. The confluence of Los Trancos Creek with San Francisquito Creek occurs just below Piers Lane Road (between Interstate 280 and the Stanford Golf Course) in a small residential island of land belonging to Menlo Park within Stanford's lands.
In 1929 Stanford installed a diversion dam on Los Trancos Creek to its Felt Lake water storage reservoir. The dam, located just below the intersection of Arastradero and Alpine Roads, blocked access of anadromous steelhead trout (Oncorhynchus mykiss) to over 3 miles (4.8 km) of pristine upstream spawning grounds. [8] In 2009, Stanford University completed construction of a new fish screen and ladder as the previous fish ladder was an "Alaska Steep Pass" designed for much higher flows. [9] The upper watershed is wholly protected within the Los Trancos Open Space Preserve just northwest of Page Mill Road and east of Skyline Boulevard. Spawning steelhead in Los Trancos Creek below the Felt Lake diversion dam vary from zero in drought years to several hundreds in wetter years and occurs from February to April. Steelhead spend two years in freshwater before heading to the Bay and field studies in the Stanford portion of Los Trancos Creek have found hundreds of young trout ranging from ~140 per mile to nearly 600 per mile. [10]
From 2016 through 2020, a pair of bald eagles (Haliaeetus leucocephalus) has nested in a large eucalyptus tree near Felt Lake and the Pearson-Arastradero Preserve. [11]
Excellent hiking from the Piers Lane parking area on Alpine Road crosses over San Franciscquito Creek and Los Trancos Creek just above their confluence and proceeds to the Stanford Dish. It is open from sunrise to sunset and no bicycles or dogs are allowed. [12]
The Coal Mine Ridge of Portola Valley Ranch has many walking (closed to biking) trails. [13]
The headwaters of Los Trancos Creek are easily accessed from Page Mill Road in the Los Trancos Open Space Preserve of the Midpeninsula Regional Open Space District and include the Lost Creek Trail, the San Andreas Fault Trail, the Page Mill Trail and Los Trancos Trail. [14]
The Santa Clara River is an 83 mi (134 km) long river in Ventura and Los Angeles counties in Southern California. It drains parts of four ranges in the Transverse Ranges System north and northwest of Los Angeles, then flows west onto the Oxnard Plain and into the Santa Barbara Channel of the Pacific Ocean.
Los Trancos Open Space Preserve is a 274-acre (1.11 km2) open space preserve, located in San Mateo and Santa Clara Counties, California, near Los Altos Hills, California. The preserve contains about 5 miles (8 km) of hiking trails, of which 2.1 miles (3.4 km) are open to equestrians, and none are open to bicycles.
Arastradero Preserve, officially known as Enid W. Pearson–Arastradero Preserve, is a 622 acres nature preserve that protects most of the Arastradero Creek watershed, including its ephemeral Mayfly Creek tributary. It also includes the upper reach of the Felt Creek tributary to Stanford's Felt Reservoir. The preserve is owned and operated by the City of Palo Alto, California. The main parking lot hosts an interpretive center and is located at 1530 Arastradero Road.
San Francisquito Creek is a creek that flows into southwest San Francisco Bay in California, United States. Historically it was called the Arroyo de San Francisco by Juan Bautista de Anza in 1776. San Francisquito Creek courses through the towns of Portola Valley and Woodside, as well as the cities of Menlo Park, Palo Alto, and East Palo Alto. The creek and its Los Trancos Creek tributary define the boundary between San Mateo and Santa Clara counties.
San Mateo Creek is a perennial stream whose watershed includes Crystal Springs Reservoir, for which it is the only natural outlet after passing Crystal Springs Dam.
San Gregorio Creek is a river in San Mateo County, California. Its tributaries originate on the western ridges of the Santa Cruz Mountains whence it courses southwest through steep forested canyons. The San Gregorio Creek mainstem begins at the confluence of Alpine and La Honda Creeks, whence it flows 12 miles (19 km) through rolling grasslands and pasturelands until it meets the Pacific Ocean at San Gregorio State Beach. It traverses the small unincorporated communities of La Honda, San Gregorio, Redwood Terrace and Sky Londa.
Adobe Creek, historically San Antonio Creek, is a 14.2-mile-long (22.9 km) northward-flowing stream originating on Black Mountain in the Santa Cruz Mountains. It courses through the cities of Los Altos Hills, Los Altos, and Palo Alto on its way to the Palo Alto Flood Basin and thence to southwestern San Francisco Bay in Santa Clara County, California, United States. Historically, Adobe Creek was a perennial stream and hosted runs of steelhead trout entering from the Bay, but these salmonids are now blocked by numerous flood control structures, including a tidal gate at the creek's mouth and a long concretized rectangular channel culminating in an impassable drop structure at El Camino Real. The co-founders of Adobe Systems both lived on Adobe Creek.
Permanente Creek is a 13.3-mile-long (21.4 km) stream originating on Black Mountain in Santa Clara County, California, United States. Named by early Spanish explorers as Arroyo Permanente or Río Permanente because of its perennial flow, the creek descends the east flank of Black Mountain then courses north through Los Altos and Mountain View, discharging into southwest San Francisco Bay historically at the Mountain View Slough but now virtually entirely diverted via the Permanente Creek Diversion Channel to Stevens Creek and Whisman Slough in San Francisco Bay.
Hale Creek is a short stream originating in the foothills of Los Altos Hills, California in Santa Clara County, California, United States. Its source is in the Rancho San Antonio Open Space Preserve, west of Neary Quarry. The creek flows northeasterly 4.6 miles (7.4 km) through the cities of Los Altos Hills, Los Altos, and Mountain View before joining Permanente Creek.
Matadero Creek is a stream originating in the foothills of the Santa Cruz Mountains in Santa Clara County, California, United States. The creek flows in a northeasterly direction for 8 miles (13 km) until it enters the Palo Alto Flood Basin, where it joins Adobe Creek in the Palo Alto Baylands at the north end of the Mayfield Slough, just before its culmination in southwest San Francisco Bay. Matadero Creek begins in the city of Los Altos Hills, then traverses the Stanford University lands and Palo Alto.
Searsville Dam is a masonry dam in San Mateo County, California that was completed in 1892, one year after the founding of Stanford University, and impounds Corte Madera Creek to form a reservoir known as Searsville Reservoir or Searsville Lake. Searsville Dam is located in the Jasper Ridge Biological Preserve and is owned and operated by Stanford University. Neighboring cities include Woodside and Portola Valley, California.
Corte Madera Creek is a 7.3-mile-long (11.7 km) creek that flows north-northwest to Searsville Dam and then joins with Bear Creek to form San Francisquito Creek in California.
Bear Creek, or Bear Gulch Creek, is a 6.6-mile-long (10.6 km) southeastward-flowing stream originating north of the summit of Sierra Morena in the Santa Cruz Mountains, near the community of Kings Mountain in San Mateo County, California, United States. It flows through the town of Woodside. Bear Creek and Corte Madera Creek join to become San Francisquito Creek in the Jasper Ridge Biological Preserve at Stanford University.
Arastradero Creek is a mainly seasonal 2.4-mile-long (3.9 km) generally north by northeastward-flowing stream originating in the Palo Alto foothills of the Santa Cruz Mountains in Santa Clara County, California, United States. It is almost wholly protected by the Pearson–Arastradero Preserve, before joining Matadero Creek where its waters descend to San Francisco Bay.
Martin Creek, known locally as Dennis Martin Creek, is a 1.4-mile-long (2.3 km) north by northeastward-flowing stream originating just east of Skyline Boulevard in the Santa Cruz Mountains, near the community of Skylonda in San Mateo County, California. It flows through the town of Woodside before crossing Portola Road and joining Sausal Creek on Stanford University lands just across the border from Woodside. Sausal Creek enters Searsville Reservoir, which flows to San Francisco Bay via San Francisquito Creek.
Barron Creek is a 5.8-mile-long (9.3 km) northward-flowing stream originating in the lower foothills of the Santa Cruz Mountains in Los Altos Hills in Santa Clara County, California, United States. It courses northerly through the cities of Los Altos Hills and Palo Alto, before joining Adobe Creek just south of U.S. Highway 101. As Adobe Creek, its waters continue northwards to southwest San Francisco Bay after crossing under Highway 101 and traversing the Palo Alto Flood Basin.
Alambique Creek, or Arroyo Alembique, is a 2.7-mile-long (4.3 km) stream located in San Mateo County, California, in the United States. It is a tributary to Corte Madera Creek and is part of the San Francisquito Creek watershed.
Sausal Creek is a 3.0-mile-long (4.8 km) northwesterly-flowing stream originating in Portola Valley along the northeastern edge of the Windy Hill Open Space Preserve in the eastern foothills of the Santa Cruz Mountains, in San Mateo County, California, United States. After being joined by Alambique Creek it flows through Middle Searsville Marsh/Pond before ending at its confluence with Corte Madera Creek in a natural marsh above Searsville Reservoir on Stanford University lands. Below Searsville Reservoir and Dam, Corte Madera Creek joins with Bear Creek to form San Francisquito Creek and flows to San Francisco Bay.
West Santa Clara is an unincorporated census county division (CCD) located on the eastern side of the Santa Cruz Mountains in northwest Santa Clara County, California. The area covers approximately 50 square miles (130 km2), much of it open space, and contains Boronda Lake, Felt Lake, and Lake Ranch reservoirs, as well as Sanborn and Stevens Creek county parks. The Foothills, Los Trancos, Monte Bello, Pearson-Arastradero, Picchetti Ranch, Rancho San Antonio and Saratoga Gap preserves are also located in the area.
Alamitos Creek or Los Alamitos Creek is a 7.7-mile-long (12.4 km) creek in San Jose, California, which becomes the Guadalupe River when it exits Lake Almaden and joins Guadalupe Creek. Los Alamitos Creek is located in Almaden Valley and originates from the Los Capitancillos Ridge in the Santa Cruz Mountains, near New Almaden. This creek flows through the Valley's Guadalupe Watershed, which is owned by the Santa Clara Valley Water District. The creek flows in a generally northwesterly direction after rounding the Los Capitancillos Ridge and the town of New Almaden, in the southwest corner, before ambling along the Santa Teresa Hills on northeast side of the Almaden Valley. Its environment has some relatively undisturbed areas and considerable lengths of suburban residential character. Originally called Arroyo de los Alamitos, the creek's name is derived from "little poplar", "alamo" being the Spanish word for "poplar" or "cottonwood".
Also see: Los Trancos Woods