The "Valley of the Little Captains" or Rancho Cañada de los Capitancillos is named for the cañada, or valley, through which Guadalupe Creek courses.[3] The river was once used for recreation prior to the removal of the Guadalupe Dam.[citation needed]
Watershed and course
The Guadalupe Creek subwatershed drains 14.8 square miles (38 km2).[4] Heading downstream east from the peak of Mount Umunhum, Guadalupe Creek is joined on the left by Rincon Creek,[5] then on the right by Los Capitancillos Creek[6] before reaching Guadalupe Reservoir. Guadalupe Dam,[7] built in 1935, formed the reservoir. The main purpose of the reservoir is to capture runoff from winter storms to recharge in the Alamitos percolation pond system during the summer.[8]
Below Guadalupe Dam, Guadalupe Creek follows Hicks Road, and just below the intersection of Reynolds Road is joined on the left first by perennial Hicks Creek (which originates at Cherry Springs and is alternatively known as Reynolds Creek and Cherry Springs Creek) on the northern side of El Sombroso Peak.[4][9][10][11] Hicks Creek has a small perennial tributary, Cherry Springs Creek, which originates at Cherry Springs Pond and flows into Hicks Creek from the west.[12][13] The next Guadalupe River tributary is Pheasant Creek,[14] which runs between Pheasant and Wagner Roads to join Guadalupe Creek from the left. At the intersection of Shannon Road and Hicks Road, Guadalupe Creek is joined next from the left by Shannon Creek.
Further downstream is Masson Dam, built in 1964, a small diversion dam about 1.3 miles (2.1 km) upstream of Almaden Expressway. The dam conveys water into the Los Capitancillos percolation ponds continually, unless Guadalupe Reservoir spills, in which case diversion operations terminate until the rainy season ends. In 1999, Masson Dam, which had been a complete barrier to fish passage, was removed and then re-built, along with a fish ladder which was completed in 2000.[8] Completed in 1962 and reconstructed in 1964, the Los Capitancillos percolation ponds occupy about 63 acres, from Almaden Expressway (east) to Camden Avenue (west).
Guadalupe Creek crosses Almaden Expressway just before joining Los Alamitos Creek at Lake Almaden, where their confluence forms the beginning of the mainstem Guadalupe River. Lake Almaden was historically a meadow but was formed by a gravel removing quarry operation. Guadalupe Creek has been entirely earthen since a short 500 foot section of concrete channel was removed near its confluence with Pheasant Creek.
Ecology
Steelhead trout (Oncorhynchus mykiss) spawned historically in Guadalupe Creek and its Pheasant Creek and Hicks (Cherry Springs) Creek tributaries through the 1950s[15] but construction of Masson Dam formed an impassable barrier. Although it is not clear whether steelhead use the dam's fish ladder (constructed in 2000), resident rainbow trout (the landlocked form of steelhead trout) persist in the upper Guadalupe Creek above the dam.[15] A 2014-2015 steelhead trout survey found "Guadalupe Creek above Hicks Road had the longest contiguous area of flowing freshwater" with appropriate conditions for residence of O. mykiss in the Guadalupe River watershed, with the highest trout catch near the mouth of Pheasant Creek.[16]O. mykiss collected above and below Guadalupe Reservoir have genetics similar to federally threatened Central California Coast Steelhead DPS distinct population segment (DPS) with no evidence of introgression from hatchery fish, despite previous stocking.[17]
Observation with a Vaki Riverwatcher fishcounter installed at the Masson Dam fish ladder during the 2006-2007 and 2007-2008 spawning seasons confirmed that steelhead trout, Pacific lamprey (Lampetra tridentata), and Sacramento sucker (Catostomus occidentalis), and possibly a Chinook salmon (Oncorhynchus tshawytscha) ascended above it.[18] This is consistent with an historic observer account of steelhead and salmon being caught by the Beltran residence where Shannon Road connects with Hicks Road, although this was likely prior to the construction of Masson Dam. There has been no fish counter installed at Masson Dam since 2008.
Guadalupe Creek is impaired (303(d) listed) by mercury contamination. Historically, workers disposed of roasted mercury mining wastes, called calcines, and other waste in or near Guadalupe Creek and Los Alamitos Creek so that waste materials would be transported downstream by winter flows. Guadalupe Reservoir covers a former mercury ore processing area. Calcines and other mining wastes are still present along the banks of Guadalupe Creek above Camden Avenue, along the banks of upper Guadalupe Creek near the former Guadalupe Mine outside of the Almaden Quicksilver County Park. A partly vegetated mining waste pile is present at Hicks Flat on the opposite side of Guadalupe Creek from the main mine.[4]
A half-mile stretch of Guadalupe Creek between Almaden Expressway and Masson Dam was restored in 2001 as mitigation for the downtown San Jose flood control project. Restoration included removal of mercury-contaminated sediments and recreation of a meandering stream course with native vegetation.[4]
^U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National MapArchived 2012-03-29 at the Wayback Machine, accessed April 11, 2013
^ abcGuadalupe Creek (Report). Santa Clara Valley Water District. Archived from the original on 2014-08-08. Retrieved 2013-05-11.
^Sowers, Janet M.; Givler, Robert W. (2006). Creek & Watershed Map of South San Jose (Report). Oakland, CA: Oakland Museum of California. Retrieved March 9, 2023.
^Jason Nishijima; Lisa Porcella; David Salsbery (April 2009). Masson Fishway 2007-2008 Monitoring Report and Alamitos and Masson Fishway 2003-2008 Summary Report, Project No. 30102001 (Report). San Jose, California: Valley Water.
