Permanente Creek


Permanente Creek is a stream originating on Black Mountain in Santa Clara County, California, United States. It is the namesake for the Kaiser Permanente health maintenance organization. Named by early Spanish explorers as Arroyo Permanente or Rio Permanente because of its perennial flow, the creek descends the east flank of Black Mountain then courses north through Los Altos and Mountain View culminating in southwest San Francisco Bay historically at the Mountain View Slough but now partly diverted via the Permanente Creek Diversion Channel to Stevens Creek and the Whisman Slough in San Francisco Bay.

History

The Ohlone Indians lived in the area for over 3,000 years prior to the arrival of the Europeans. A large village, known as Partacsi, was located in this general area. An expedition led by Colonel Juan Bautista de Anza passed through this area in March 1776 as he forged the first overland route from Monterey to San Francisco Bay. Mission Santa Clara de Asis was founded in October of the same year, where many of the local Indians were taken. Governor Alvarado granted Rancho San Antonio de Padua to Juan Prado Mesa in 1839. This rancho was bounded by Adobe Creek to the north and Stevens Creek to the south, and included Permanente Creek. On a diseño of Rancho San Antonio in 1839 Permanente Creek is shown as Arroyo Permanente. Mesa had been a soldier at the Presidio of San Francisco since 1828, served as a corporal in the Santa Clara Guard, and had won fame as a soldier and Indian fighter. Mesa died in 1845.
Permanente Creek is also the namesake for Kaiser Permanente. Bess Kaiser and her spouse, industrialist Henry J. Kaiser, had a lodge on the creek's headwaters above the large Permanente Quarry and Cement Plant, and, in 1945, Bess felt that the name of their attractive and dependable stream would be a good name for their medical program at the shipyards. That medical program became Kaiser Permanente.

Watershed

Permanente Creek consists of approximately of channel draining a watershed area of. From its origination at in headwaters protected by the Midpeninsula Regional Open Space District just north of the peak of Black Mountain, Permanente Creek descends along the Permanente Quarry, and continues easterly through unincorporated County land for about five miles, then turns to the north at the base of the foothills and continues another eight miles along the valley floor. It has two major tributaries, the West Fork Permanente Creek and Hale Creek. West Fork Permanente Creek and its Wildcat Canyon tributary were formerly known as Ohlone Creek. West Fork Permanente Creek begins on the east side of Ewing Hill, and runs easterly until it reaches the connector from the Chamise and Rogue Valley Trails where an earthen dam forms High Meadow Pond. Below the pond, the West Fork is joined by long Wildcat Canyon Creek at Deer Hollow Farm, then continues on its run to the Permanente Creek mainstem which it joins south of Interstate 280.
Flows are perennial in the upper watershed but ephemeral on the valley floor, with two exceptions: the portion of the Permanente Creek mainstem between Foothill Expressway and Interstate 280, and the Hale Creek tributary. The perennial reaches of these creeks share the same perennial nature as a similar reach on nearby Adobe Creek.

Diversion channel

Except for sakrete banking and several weirs, Permanente Creek's upper mainstem runs about in a relatively unmodified natural channel until reaching Portland and Miramonte Avenues at the north end of Heritage Oaks Park. Here the creek enters a concrete trapezoidal channel constructed by the Santa Clara Valley Water District. Just before reaching the rear of Blach Intermediate School, it becomes the Permanent Creek Diversion Channel, built by the SCVWD in 1959, and runs a total of, continuing due east until passing in a culvert beneath east under Highway 85 to Stevens Creek. A floodgate is closed every winter that diverts virtually all winter flows east to Stevens Creek, preventing high winter floodwaters from flowing north in the original creek channel through dense residential areas. Only during high floods can a portion of the creek's waters surmount the floodgate and return to the original channel. Therefore, the Diversion Channel effectively reconnects Permanente Creek to the Stevens Creek watershed. This recapitulates the 1862 Allardt Map of the San Francisco & San Jose Railroad which shows Permanente Creek as a tributary of Stevens Creek . This is significant ecologically, because Stevens Creek still hosts an anadromous steelhead trout run. Although steep drops in the Diversion Channel are impassable barriers to upstream fish migration, modifications to the Diversion Channel would allow trout to run to the upper Permanente Creek watershed. The Diversion Channel essentially changes the total length of Permanente Creek from to San Francisco Bay to ending at its junction with Stevens Creek just past Highway 85. However, Hale Creek still flows to the channelized lower reaches of Permanente Creek.

Lower mainstem

The original creek channel below the floodgate in the Diversion Channel, now severely depleted of water, runs north another to its confluence with Hale Creek just upstream from McKelvey Park. Permanente Creek's original channel then goes on to pass under U. S. Highway 101, along the west side of the Google campus, and out to the Bay at the Mountain View Slough just east of Shoreline Park, the latter built on a reclaimed San Francisco garbage dump in 1983. This lowest part of the creek historically disappeared into the marshland before reaching the Bay, and its channel was extended to the Bay in the nineteenth century. The creek must have been hydrologically connected to the Bay at times of high winter flows since steelhead trout were able to access Permanente Creek historically. Saltwater is pumped from Charleston Slough into Shoreline Lake and from there it flows to Permanente Creek and then back into the Bay. The Mountain View Slough carries flows to the Bay between former salt ponds A1 and A2W. The levees around these ponds will be breached and opened to the Bay as part of the South Bay Salt Pond Restoration Project Phase II.
The Santa Clara Valley Water District plans to excavate as much as down to create flood detention basins to protect homes from a 100-year Permanente Creek flood at Cuesta Park Annex, Blach Intermediate School, McKelvey Park and Rancho San Antonio County Park. Despite considerable community opposition, the SCVWD Board approved the decision to go ahead on June 17, 2010. The Blach School Board voted against use of school property for a detention basin but construction permits are being sought as of 2016 for the McKelvey Park and Rancho San Antonio Park basins. Construction of the McKelvey Park detention basin and recreational facilities was completed in February 2020. Construction at Rancho San Antonio Park is planned to include a 15-foot deep basin and new park infrastructure.

Ecology

Federally threatened California red-legged frogs inhabit the upper watershed of Permanente Creek and the US Fish and Wildlife Service in 2017 asked the Army Corps of Engineers to assure that sufficient riparian habitat, specifically near ponds 14 and 21 along the Permanente Quarrry, would be set in a conservation easement to ensure their survival. In fact, a 2011 biological resources assessment of the quarry property found six California special status wildlife species, including the California red-legged frog, dusky-footed woodrat

Pollution

Mercury

The cement plant at the Permanente Quarry is responsible for 29% of total Bay Area airborne mercury emissions and was shown to impact a rural site, Calero Reservoir, away. Mercury, a neurotoxin and pollutant which is concentrated in the aquatic food web, was found to be 5.8 to 6.7 times higher in precipitation near the cement plant than at a control location away. A 2011 study showed a significant geographic association between the occurrence of autism in local school districts, such as the Cupertino Union School District, and higher levels of ambient mercury generated by coal-fired power plants in Bexar County, Texas and the Permanente Quarry cement plant in Santa Clara County, California.

Selenium discharges

Groundwater fills the current quarry and is pumped into Permanente Creek. Selenium pollution in the creek downstream from the quarry ranged from 13 to 81 micrograms/liter. A North Quarry water sample in January 2010 had a dissolved selenium concentration of 82 μg/L, indicating that the quarry is the source of the selenium pollution. Selenium is bioaccumulated in the aquatic food web. Safety standards for selenium concentrations in fresh water are 5 μg/L under the California Toxics Rule in 2000 and 2012.

Sediment discharges

activities related to quarry operations and the cement plant have resulted in sediment discharges into Permanente Creek that are 3.5 times what would be expected under normal conditions. Sediment loads in the upper Permanente Creek mainstem are 15 times those in the West Fork Permanente Creek, which drains mostly parkland. These sediment loads could threaten the resident rainbow trout population in the creek.

Recreation

Above Interstate 280 a large section of the creek mainstem and all of the West Fork Permanente Creek tributary, and the Ohlone Creek sub-tributary, is protected by Rancho San Antonio County Park and Rancho San Antonio Open Space Preserve. The Open Space Preserve, combined with the adjoining County Park, in area and contains of hiking trails. A one-mile walk from the County Park's main parking lot leads to the historic 10-acre Deer Valley Farm on the West Fork Permanente Creek.
There is a trail that runs along the creek, beginning at the historic Rengstorff House in Shoreline Park where it is connected to the San Francisco Bay Trail. The Permanente Creek Trail runs from there south to West Middlefield Road.

Gallery