In 1993, archeologist Mark Hylkema documented eight different Native American sites on the Andresen Ranch along the lower North Fork Pacheco Creek, dating from 1000 B.C. to 500 A.D. These included multiple human burials, both adult and juvenile. He concluded that the interior of the Diablo Range north of Pacheco Pass was extensively occupied. Although Central ValleyYokuts may have utilized this area, archeologist E. Breck Parkman, who studied sites along upper North Fork Pacheco Creek, summarized evidence that the primary occupants were Ohlone, of the Tomoi, Locobo, and Cobo Ohlone peoples. These peoples were removed to Missions Santa Clara and Santa Cruz between 1800 and 1808.
Watershed
The North Fork Pacheco Creek has two main tributaries. Furthest upstream is the Mississippi Creektributary of North Fork Pacheco Creek. It is long and has an impoundment above elevation. Mississippi Creek sources on Bear Mountain on the northern side of Henry W. Coe State Park. The North Fork Pacheco Creek also receives the long East Fork Pacheco Creek, at Chimney Rock before reaching Pacheco Reservoir and Dam, the latter just north of Highway 152. The mouth of North Fork Pacheco Creek is at its confluence with South Fork Pacheco Creek at an elevation of 430 feet / 131 meters where it forms the head of the Pacheco Creek mainstem west of Pacheco Pass. In 2019, the U.S. Bureau of Reclamation released a draft environmental report that the 100-foot earthen Pacheco Creek dam be replaced with a $1.1 billion dam that would increase reservoir capacity from 5,500 acre-feet to 140,000 acre feet, making it larger than Anderson Reservoir, currently the largest reservoir in Santa Clara County.. However, environmentalists have proposed a smaller dam on only the East Fork Pacheco Creek, so that only one stream would be blocked instead of two, and enabling the opening of the North Fork Pacheco Creek to spawning runs of steelhead trout to the perennial waters in the upper watershed within Henry Coe State Park.
Ecology
Pacheco Reservoir is an impassable barrier to in-migrating steelhead trout, preventing access to the nearly of stream consisting of North Fork Pacheco Creek, Mississippi Creek and East Fork Pacheco Creek. However, resident rainbow trout successfully rear in fast-water habitats in the headwaters but cannot in-migrate because of the dam, likely leading to genetic inbreeding depression, as in other nearby streams with passage barriers. In many years in late spring, prior to reservoir releases for agriculture, low stream flows and high water temperatures severely impact steelhead fry and small juveniles. Other native fish in North Fork Pacheco Creek include Monterey sucker and Sacramento pikeminnow.
