The Red Hills Management Area consists of 7,100 acres (slightly more than 11 square miles) of public land located near the intersection of State Highways 49 and 120, just south of the historic town of Chinese Camp in Tuolumne County.
The Red Hills came into Federal ownership along with most of California with the signing of the Treaty of Guadalupe Hidalgo in 1848 that officially ended the war with Mexico. They are still in Federal ownership simply because no one wanted the land in the days when it was Government policy to dispose of the public domain. There was little or no gold associated with the serpentine rocks, and crops wouldn't grow properly in the serpentine-derived soil.
A county-maintained road, dating back to 1849, runs through the heart of the Red Hills.
In recent times the Red Hills have mostly been used for recreation. The main recreation uses have been target shooting off-road vehicle driving, camping, hunting, hiking, horseback riding, nature study, wildflower viewing, and hobby prospecting. To protect the fragile biological resources of the area, in 1991 target shooting and off-road vehicle use were prohibited on public land in the Red Hills.
Elevations within the Red Hills vary between 750 and 1,750 feet above sea level. Slopes of the hills themselves vary from about 30% to 75%.
Average rainfall for the area is roughly between 25 and 30 inches per year. Occasionally, there is a light snowfall. Typical of California, most precipitation occurs between November and April. During the winter, temperatures can range between 14 degrees F. to 82 degrees F. with an average of 47 degrees F. Summertime temperatures range between 35 and 109 degrees F., with an average of 74 degrees F.
The Red Hills Management Area is located within the western tectonic block of the Sierra Nevada metamorphic belt. Within this block are Upper Jurassic volcanic and sedimentary rocks of island arc derivation which were highly deformed and weakly metamorphosed during the Nevada orogeny. These rocks were then intruded by plutons associated with the emplacement of the Sierra Nevada batholith, east of the metamorphic belt.
The Management Area includes much of the Tuolumne ultramafic complex, one of the largest exposures of serpentine rocks in the Sierra Nevada metamorphic belt. Nearly the entire area is underlain by dunite, a variety of peridotite consisting of dark green olivine and minor chromite, which as been partly or entirely serpentinized to antigorite magnesite-magnetite. The dunite intruded into andesite pillow breccias and flows of the Peñon Blanco volcanic formation, which crops out near the northeast and southern boundaries of the Management Area. The intrusion of ultramafic material occurred along crustal weaknesses associated with the Bear Mountain fault, a northwestward trending thrust fault that dips steeply to the northeast, and has over 10,000 feet of vertical displacement. The fault zone is on the southwestern boundary of the Management Area, and is believed to have once penetrated the earth's crust down to the mantle, a probable source of the peridotite.
Other geologic features of the area include northeastward trending dikes that consists of massive, dark brown, hornblende-plagioclase diorite which intruded into the dunite bedrock. A swarm of several dikes occurs in the southeast portion of the Management Area. Some of the dikes exceed one mile in length. Amphibolite and chert tectonic blocks also occur in the dunite near the area's southern and western boundaries.
Tertiary and Pleistocene alluvium consisting of sand, gravel, pebbles, and cobbles has accumulated in Six Bit and Poor Man's Gulches in the northern and eastern portions of the Management Area.
Although the potential for the development of mineral resources in the Red Hills is limited, deposits of chromite and magnesite occur in serpentine rocks. Placer gold occurs in stream channel deposits within the natural area, primarily Six Bit Gulch and Poor Man's Gulch, mostly washed in from the north.
From the 1860s to the 1940s, roughly 10,000 tons of chromite ore and several hundred tons of crude magnesite ore were mined. Most of the chromite came from the McCormick Mine, located northwest of the Management Area. All of the magnesite production in Tuolumne County occurred in the 1920s and came from two sites in the northern portion of the Red Hills. Currently, there is no market for crude magnesite in the United States.
The placer gold produced from this district was recovered by ground sluicing and hydraulic mining in earlier years, and by dragline dredging in the 1930s and 1940s. In the 1850s, during the great California Gold Rush, Chinese laborers, with their legendary patience and thoroughness, mined much of the placer gold within Six Bit Gulch, a major drainage channel that courses through the natural area. The dredging of Six Bit Gulch and Poor Man's Gulch produced over $100,000 worth of gold, but the mining operations were reportedly not profitable. Because lode gold is not usually associated with serpentine bedrock, the intermittent streams which originate within the Red Hills contain little, if any, placer gold.
The major soil type is the Delpiedra Series. Henneke and Fancher soils, also derived from serpentine parent material, are also present.
The Red Hills are vegetated mostly by a foothill pine-buckbrush chaparral/woodland. Virtually the only tree species in the Red Hills is foothill pine (Pinus sabiniana), which is found throughout the Red Hills in low densities. Buckbrush (Ceanothus cuneatus) comprises a majority of the shrub cover. Other shrubs include Toyon (Heteromeles arbutifolia), coffee berry (Rhamnus californica tomentella), chamise (Adenostoma fasciculatum), hollyleaf redberry (Rhamnus crocea ilicifolia), California yerba santa (Eriodictyon californicum) and manzanitas (Arctostaphylos spp.).
Native perennials constitute a large percentage of the grass cover in the Red Hills. This is in contrast to similar elevations in the foothills, without serpentine substrates, where native perennials have been mostly replaced by exotic annuals. Important native perennial species include California oniongrass (Melica californica), big squirreltail (Sitanion jubatum) and pine bluegrass (Poa secunda). Disturbed areas, including burned areas, have a typical array of Mediterranean annual grasses.
Herbaceous plants provide a spectacular wildflower bloom in the spring that attracts tourists, amateur naturalists, and classes from educational institutions. Although most of the species comprising the display are widespread on and off serpentine, some (in addition to the rare species discussed below) are strict serpentine endemics (e.g., Streptanthus polygaloides).
Sensitive plants: Five plants which occur on the public lands of the Red Hills are considered sensitive species by BLM due to their rarity. Two of the plants have been proposed for listing under the Endangered Species Act indicating that the U.S. Fish and Wildlife Service feels it has accumulated sufficient evidence to list these species. These plants are the California verbena (Verbena californica), Rawhide Hill onion (Allium tuolumnense). A third plant species, Layne's butterweed (Senecio layneae), has already been listed as a threatened species.
California verbena is a Red Hills endemic, meaning it is found nowhere else in the world. Its distribution in the Red Hills is confined to the short stream reaches that remain moist year round because of ground water seepage.
The Rawhide Hill onion has many, mostly small, colonies in the Red Hills. Rawhide Hill onion is confined to areas with sparse vegetation, south facing slopes with shallow soils, and intermittent drainages.
Senecio layneae is the only federally listed plant species in the Red Hills at this time. There are only a few very small occurrences of this member of the sunflower family in the Red Hills. Here as elsewhere, this species is often associated with disturbances like roadcuts. Senecio layneae is also found in El Dorado County on serpentine and gabbro.
Two plants that had been designated as federal candidate category 2 species were eliminated from the list of candidate species when the U.S. Fish and Wildlife Service changed its rules for the inclusion of species as candidates in 1996. Congdon's lomatium (Lomatium congdonii) and the Red Hills soaproot (Chlorogalum grandiflorum) are locally common throughout the Red Hills favoring north slopes and ridgetops respectively. Congdon's lomatium is only known from the Red Hills and the Peoria Valley area. Red Hills soaproot is also found in El Dorado County on serpentine and gabbro.
An additional species proposed for federal listing occurs on private lands just west of Chinese Camp and within a mile of the public land. Chinese Camp brodiaea (Brodiaea pallida) grows near a low gradient drainage in soils that remain wet late into the growing season. This species has not been located on the public lands of the Red Hills.
Another plant, Hoover's butterweed (Senecio clevelandii var. heterophyllus) has been included on the California Native Plant Society's Watch List. It grows with the California verbena in riparian zones. It may be recognized as a separate taxon that is endemic to the Red Hills, or it may be included as a single taxon with plants found in the Coast Ranges.
In the Red Hills buckbrush and other shrubs provide browse and seeds for small populations of mammals, including mule deer, jackrabbits, rodents. Coyotes, bobcats and fox can also be found in the Red Hills.
88 bird species have been observed in the Red Hills. Some common species include mourning dove, acorn woodpecker, ash-throated flycatcher, scrub jay, wrentit, plain titmouse, bushtit, Bewick's wren, and house finch. Valley quail and mourning doves are the major game birds in the Red Hills. An abundant insect population supports insectivorous birds including western kingbirds, ash- throated flycatcher, tree swallows, barn swallows, black phoebes, and others. Raptors include the red-tailed hawk, Cooper's hawk, prairie falcon, and great horned owl. Fish-eating birds seen in the Red Hills include the belted kingfisher and great blue heron. Roadrunners can also be found.
Reptiles and amphibians are rarely observed in the Red Hills but interestingly two rare species are represented (see below).
Fish in the Red Hills, found in Six Bit Gulch and Poor Man's Creek, include the green sunfish, large-mouth bass, Sacramento sucker, and the mosquito fish. These fish are predators or competitors with the Red Hills roach, a rare taxon (discussed below). The presence of these mostly introduced species may limit the roach population.
Rare fauna: Four sensitive species of animals are known from the Red Hills. Wintering bald eagles roost along the shores of Don Pedro Reservoir and have been observed where Six Bit Gulch enters the lake. As many as 20 bald eagles have been sighted during the winter on the shores of Don Pedro Reservoir, roosting in stands of foothill pines.
Although the Red Hills has no perennial streams, it has a number of intermittent streams that have spring fed reaches and pools. Two sensitive riparian animal species are associated with these areas, Hesperoleucus symmetricus (California roach, a minnow; the distinctive Red Hills population has been called the Red Hills roach) and Rana boylii (foothill yellow legged frog).
The Red Hills roach is found in abundance in several pools of permanent water located along the intermittent streams which drain into Six Bit Gulch and Poor Man,s Gulch. It is thought that the permanent pools are spring-fed. During the dry part of the year the fish are confined to these permanent pools surviving in warm shallow water until spring when they move upstream to spawn. A recent study by ichthyologists at the University of California, Davis, and the California Department of Fish and Game has indicated that the Red Hills variety of California roach has unique morphologic characteristics, which make them noticeably different from other roach populations, notably a chisel lip. The chisel lip is used to scrape algae, a major food source, off submerged rocks.
Up until 1996 the U.S. Fish and Wildlife Service had recognized the Red Hills roach as a candidate (category 2, now eliminated) for listing under the Endangered Species Act. The isolated nature of the population of the Red Hills roach due in part to past and continuing habitat degradation has led some researchers to be concerned about the roach's long-term survival. The presence of a number of introduced fish species such as green sunfish, large mouth bass and mosquito fish may limit the roach population by predation and/or competition.
The foothill yellow-legged frog has been found in the western portion of the Red Hills in the Andrews Creek drainage. The western pond turtle has been found in the eastern portion of the Red Hills in Poor Man's Gulch. Both are rare species, formerly candidates for federal listing.
Compared to surrounding areas, the Red Hills Management Area has fewer cultural resources.
Prior to the Gold Rush of 1849, the Management Area was probably lightly populated by the Central Sierran Miwok people. There are several grinding rocks near one of the intermittent streams, but no occupation sites have been found. This is in contrast to nearby areas where several occupation sites have been recorded. The Red Hills were probably not heavily used by the Miwok people because of the scarcity of game and the lack of acorns. It is possible that the Miwok people may have utilized the riparian areas along Six Bit Gulch, however, any trace of that use was likely wiped out years ago by placer mining activities, as were so many other sites in the Mother Lode region.
Some evidence of Chinese habitation has been found at a few scattered sites. The first Chinese miners arrived in the vicinity during 1849. Most of their activity was centered around the town of Chinese Camp to the immediate north of the Red Hills. A large fight between two feuding Chinese factions--a Tong War--occurred in 1856, supposedly just to the south of the Red Hills in the vicinity of the historic Crimea House.
Red Hills Road, which bisects the study area, dates back to 1849 when it was a major route between Central Valley locations and the southern mining camps. The Crimea House, an inn which was located just to the south of the public land, provided lodging and food to early travelers. The Crimea House itself was destroyed in a fire in 1949. The site is marked by a plaque erected by the Fraternal Order of E Clampus Vitus.
An abandoned railroad grade is located in the northwestern portion of the Red Hills. It was part of the old Sierra Railroad, constructed during the 1890s, to carry freight between the main railroad lines in the central valley and the mining communities of the Mother Lode region.
Area of Critical Environmental Concern (ACEC):
The entire Red Hills Management Area has been designated as an ACEC. The purpose of the designation is to protect the rare plant species found there, the unusual serpentine soils that provide habitat for unique flora of the area, habitat for the rare minnow known as the Red Hills roach and to protect bald eagle wintering habitat.