Coyote Creek (Santa Clara County)

HistoryEdit

Coyote Creek was originally named Arroyo del Coyote by Padre Pedro Font when the de Anza Expedition reached it on Sunday, March 31, 1776.

WatershedEdit

Although it is called a "creek", Coyote Creek is actually a river draining 320 square miles (830 km²) and running 63.6 miles (102.4 km) from the confluence of its East Fork and Middle Fork to southeast San Francisco Bay. The river's main source is on Mount Sizer near Henry W. Coe State Park and the surrounding hills in the Diablo Range, northeast of Morgan Hill, California. At the base of the Diablo Range, the creek is impounded by two dams, first Coyote Reservoir and then Anderson Lake. Nine major tributaries lie within the area that drains to these two reservoirs: Canada de los Osos, Hunting Hollow, Dexter Canyon, and Larios Canyon Creeks drain to Coyote Reservoir; Otis Canyon, Packwood, San Felipe, Las Animas, and Shingle Valley Creeks drain to Anderson Lake. Coyote Reservoir Dam was built across the active 1000-ft wide trace of the Calaveras fault by the Santa Clara Valley Water District (SCVWD) between 1934–36, storing 10,000 acre feet (12,000,000 m³) of water.

From Anderson Lake, Coyote Creek continues northwards from Morgan Hill through Coyote Valley, the narrowest point between the Diablo Range and the coastal Santa Cruz Mountains, where it picks up Fisher Creek before entering San Jose. As Coyote Creek forms the eastern boundary of downtown San Jose, it winds its way into North San Jose. There, Miguelita Creek, Penitencia Creek, and Berryessa Creek are all tributaries. Coyote Creek then bypasses the Newby Island landfill and empties into the San Francisco Bay.

There is a chain of parks along Coyote Creek called the Coyote Creek Park Chain. The feasibility of a trail connecting the parks within this chain to Almaden Park was first examined in 1989.

The river is managed by the SCVWD. In 1983, torrential rains caused by el Niño resulted in significant flooding of Coyote Creek in the Alviso neighborhood. The SCVWD, with advice from Santa Clara Basin Watershed Management Initiative (WMI) stakeholders, produced a stream stewardship plan for the Coyote Creek watershed in 2002. The plan includes over sixty projects to benefit flood protection, habitat enhancement, parks, and trails.

The Silver Creek Fault runs generally parallel to Coyote Creek.

Risk of Anderson Dam failure from earthquakesEdit

Updated findings from an ongoing study of Anderson Dam were released in October, 2010 indicated that the dam could fail if a magnitude 7.25 earthquake occurred within 2 kilometers of the dam, potentially releasing a wall of water 35 feet high into downtown Morgan Hill in 14 minutes, and 8 feet deep into San Jose within three hours. In response SCVWD has lowered the water to 54% full, which is 60 feet below the dam crest. According to the SCVWD, remediation of the problem will likely require lengthy construction that would take up to six years and cost as much as $100 million.

Because Coyote Reservoir Dam was built right across the Calaveras fault and there is a substantial risk of a seismic-triggered landslide on the east side of the reservoir at the dam site, an earthquake could cause failure of this dam upstream of the Anderson Dam, and the release of water could increase risk of failure of the Anderson Dam.

2017 Coyote Creek FloodEdit

By 4:00 P.M. February 20, 2017 San Jose City opened overnight shelter for residents who choose to voluntarily evacuate their homes in low-lying areas along Coyote Creek. Subsequant days, the city started issuing mandatory and advisory evacuation areas

Habitat and wildlifeEdit

Coyote Creek has historically, and still does support the most diverse fish fauna among the Santa Clara Valley Basin watersheds. It supports 10 to 11 native fish species out of the original 18. Species known to occur currently include Pacific lamprey (Lampetra tridentata), steelhead/resident rainbow trout (Oncorhynchus mykiss), chinook salmon (Oncorhynchus tshawytscha), California roach, Hitch (Lavinia exilicauda), Sacramento blackfish (Orthodon microlepidotus), Sacramento pikeminnow, Sacramento sucker, three-spined stickleback, prickly sculpin (Cottus asper), riffle sculpin (Cottus gulosus), staghorn sculpin, and tule perch (Hysterocarpus traskii). Three species, the thicktail chub, splittail, and Sacramento perch have been extirpated from the drainage; the thicktail chub is extinct.

A 1962 report indicated that Coyote Creek, from its mouth to the headwaters in Henry Coe State Park, was an historical migration route for steelhead trout. SCVWD studies have shown that Standish Dam and percolation ponds have posed barriers to outmigrating trout. Based on these results, Standish Dam has not been installed since 2000. The on-channel percolation ponds constructed on Coyote Creek severely degrade steelhead habitat by harboring non-native fish predators, such as largemouth bass (Micropterus salmoides) which prey on salmonid fingerlings, and also by releasing warm water flows. Moving Ogier Ponds and Metcalf Percolation Ponds off-channel would significantly enhance rearing habitat for steelhead.

The Chinook salmon run in Coyote Creek may be the most viable for restoration in the South Bay, since the breeding salmon in the Guadalupe River have severely declined subsequent to installation of extensive concrete channels in the river in downtown San Jose, California by the SCVWD. These are “fall run” fish primarily adapted to the Sacramento and San Joaquin River watersheds. Since Chinook salmon spawn in early winter and juveniles migrate to the ocean in their first spring, they are able to use habitats that turn very warm or have low water quality in summer. In 2012, the Santa Clara Valley Habitat Plan reported that Chinook salmon currently spawn in Coyote Creek as well as the Guadalupe River and its tributaries.

Coho salmon (Oncorhynchus kisutch) were present in the Coyote Creek watershed until the 1950s, suggesting that some spawning and rearing habitat was located in the watershed downstream from Coyote Reservoir which was completed in 1936 (blocking access to 310 square kilometers of upstream watershed). Historically, suitable habitat for coho salmon in the Coyote Creek watershed was likely restricted to the San Felipe Creek and Upper Penitencia Creek watersheds and possibly perennial reaches of Coyote Creek, and a few spring-fed tributaries upstream from Gilroy Hot Springs. Assuming the Coyote Percolation Reservoir was not a complete barrier to coho salmon; the construction of Anderson Dam in 1950 would have eliminated any coho salmon that occurred in the San Felipe Creek watershed that now flows into Anderson Lake. However, if the Coyote Creek Percolation Reservoir were a migration barrier, then only Upper Penitencia Creek would have provided suitable habitat for coho salmon after 1934. San Felipe Creek currently contains habitat potentially suitable to coho salmon with low stream temperatures related to cool groundwater discharges in the Calaveras Fault zone. During early June and late-July 1997, the senior author recorded water temperatures within the San Felipe Creek watershed within pools containing rainbow trout between 11–13.3 °C and 14.4–17.7 °C, respectively. Zones of groundwater discharge along the Calaveras Fault zone that traverses the watershed maintain cool summer water temperatures. Upper Penitencia Creek, which enters lower Coyote Creek near its mouth and drains the steep coastal hills to the east also may have contained suitable coho salmon habitat.

A 1962 California Department of Fish and Wildlife report indicates that golden beaver (Castor canadensis subauratus) lived in Coyote Creek historically. This report is consistent with Alexander McLeod's report on the progress of the first Hudson's Bay Company fur brigade sent to California in 1829, "Beaver is become an article of traffic on the Coast as at the Mission of St. Joseph alone upwards of Fifteen hundred Beaver Skins were collected from the natives at a trifling value and sold to Ships at 3 Dollars". Physical proof of Golden beaver in south San Francisco Bay tributaries is a Castor canadensis subauratus skull in the Smithsonian Institution National Museum of Natural History collected by zoologist James Graham Cooper in Santa Clara, California on Dec. 31, 1855.

A 1995 study showed high levels of toxic substances in receiving waters and sediments along urban areas of the creek versus undeveloped areas. This correlates to the density of storm drains suggesting that the pollution is from urban run-off.