Chinese Camp District

Past Producer in Tuolumne county in California, United States with commodity Gold

Sections on this page

Identification information
Geographic coordinates
Site location context
Geographic areas
Public Land Survey System information
Commodities
Materials information
Mineral occurrence model information
Host and associated rocks
Nearby scientific data
Ore body information
Controls for ore emplacement
Economic information about the deposit and operations
Mining district
Land status
Bibliographic references
General comments
Reporter information

Geologic information

Identification information

Deposit ID	10310603
Record type	District
Current site name	Chinese Camp District

Comments on the site identification

This district encompasses an area of placer mining in and around the settlement of Chinese Camp.

Geographic coordinates

Geographic coordinates:	-120.43301, 37.87078 (WGS84)
Location accuracy	100(meters)
Relative position	Location is about 8 miles south-southwest of the downtown section of the city of Sonora.

Site location context

Political divisions (FIPS codes)

Tuolumne(county)

California(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Chinese Camp(quadrangle 1:24,000 scale)

Oakdale(quadrangle 1:100,000 scale)

San Jose(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Upper Tuolumne(hydrologic unit)

San Joaquin(hydrologic accounting unit)

San Joaquin(hydrologic subregion)

California(hydrologic region)

Geographic areas

Country	State	County
United States	California	Tuolumne

Public Land Survey System information

Meridian	Township	Range	Section	Fraction	State
Mount Diablo	001S	014E	04	SE	California

Comments on the location information

Location selected for latitude and longitude is the settlement of Chinese Camp on the USGS 7.5-minute Chinese Camp quadrangle.

Commodities

Commodity	Importance
Gold	Primary

Comments on the commodity information

Commodity Info: There is little published information on the character and conditions of the gold at this district probably because most of the placer mining was done during the gold rush when record-keeping was relatively poor.
Ore Materials: Native gold
Gangue Materials: Metamorphic rock, igneous rock, quartz

Materials information

Materials	Type of material
Gold	Ore
Quartz	Gangue

Mineral occurrence model information

Model code	119
USGS model code	39a
Deposit model name	Placer Au-PGE
Mark3 model number	54

Host and associated rocks

Host or associated Associated

Rock type Unconsolidated Deposit > Sand and Gravel

Stratigraphic age (youngest) Tertiary
Host or associated Associated

Rock type Unconsolidated Deposit > Sand and Gravel

Stratigraphic age (youngest) Quaternary

Nearby scientific data

(1)	-120.43301, 37.87078	ListMap

Economic information

Ore body information

General form Irregular

General form	Irregular

Controls for ore emplacement

Mechanical accumulation within stream-channel lag gravels, bars, and point-bar deposits as well as erosional lag on bedrock surfaces in basins (placer).

Comments on the geologic information

The Chinese Camp District is within the Sierra Nevada foothills, where bedrock consists of northerly trending tectonostratigraphic belts of metamorphosed sedimentary and volcanic rocks and associated intrusive rocks that range in age from Paleozoic to Mesozoic. The structural belts, which extend about 235 miles along the western side of the Sierra, are flanked to the east by the Sierra Nevada Batholith and to the west by sedimentary rocks of the Cretaceous and Jurassic Great Valley sequence. The structural belts are internally bounded by the Melones and Bear Mountains fault zones and are characterized by extensive faulting, shearing, and folding (Earhart, 1988).

From El Dorado County southward into Mariposa County, lode gold deposits occur in three distinct belts - the West Belt, the Mother Lode Belt, and the East Belt. The Mother Lode Belt is responsible for most of the gold produced. However, there has also been substantial gold production from the West Belt and East Belt.

The West Belt in Tuolumne County consists of sparse, widely scattered gold deposits located west of the Mother Lode vein system, which represents the Mother Lode Belt. Gold occurs in irregular quartz veins and stringers in schist, slate, granitic rocks, altered mafic rocks, and as gray ore in greenstone. The West Belt is cut by the northwest-trending Bear Mountains fault zone, which separates an assemblage of metavolcanic and metasedimentary rocks of Jurassic age on the southwest from a more disrupted and diverse assemblage of metavolcanic, metasedimentary, plutonic, ultramafic, and melange rocks on the northeast. The metavolcanic rocks consist generally of volcanic and volcanic-sedimentary rocks of island arc affinity. These rocks are mostly mafic to intermediate in composition and include flows, breccias, and a variety of layered pyroclastic rocks. Some silicic rocks are present also. Various formation names assigned to the metavolcanic assemblages include Gopher Ridge, Copper Hill, Logtown Ridge, and Penon Blanco the metasedimentary rocks are dominantly distal turbidites and hemipelagic sequences of black slate. Assigned formation names include Mariposa, Salt Spring Slate, and Merced Falls Slate.

The northwest-trending Mother Lode Belt traverses western Tuolumne County and is associated with the Melones Fault Zone. The rocks of this belt are typically metavolcanic, metasedimentary, and ultramafic, some of which have been hydrothermally altered to assemblages as described below. Mother Lode Belt mineralization is characterized by steeply dipping gold-bearing quartz veins and bodies of mineralized country rock adjacent to veins. Mother Lode veins are characteristically enclosed in Mariposa Formation slate with associated greenstone. The Mother Lode belt vein system ranges from a few hundred feet to a mile or more in width. Within the zone are numerous discontinuous or linked veins, which may be parallel, convergent, or en echelon. The veins commonly pinch and swell. Few can be traced more than a few thousand feet. Mother Lode type veins fill voids created within faults and fracture zones and consist of quartz, gold and associated sulfides, ankerite, calcite, chlorite, limonite, talc, chromium-bearing mica, and sericite. Stringer veins are commonly found in both adjacent footwall and hanging walls.

Mother Lode ores are generally low- to moderate-grade (1/3 ounce of gold or less per ton), but ore bodies can be large. Ore shoots are generally short, 200-300 feet being the average stope length. However, they persist at depth, some having been mined to several thousand feet (Clark and Lydon, 1962). Ore shoots are commonly localized at bulges in veins, shear zones, vein intersections, or near abrupt changes in strike or dip.
Wall rocks have invariably been hydrothermally altered, having been partially to completely converted to ankerite, sericite, quartz, pyrite, arsenopyrite, chlorite, and albite with traces of rutile and leucoxene (Knopf, 1929). The mineralization is usually adjacent to the veins in ground that has been fractured and contains small stringers and lenses of quartz. Locally, greenstone bodies adjacent to the quartz veins contain enough disseminated auriferous pyrite in large enough bodies to constitute what has been called "gray ore". Altered slate wall rock commonly contains pyrite, arsenopyrite, quartz, chlorite, and sericite with or without ankerite (Zimmerman, 1983).

Large bodies of mineralized schist also form low-grade ore bodies throughout the Mother Lode. This ore consists of amphibolite schist that has been subjected to the same processes of alteration, replacement, and deposition that formed the greenstone gray ores. The altered schist consists mainly of ankerite, sericite, chlorite, quartz, and albite. Gold is associated with the pyrite and other sulfides that are present. Pyrite comprises about 8 percent of the rock. The average grade of mineralized schist is about 0.1 oz per ton.

The Melones Fault zone separates the Mother Lode Belt from the East Belt. The East Belt is dominantly argillite, phyllite and phyllonite, chert, and metavolcanic rocks of Paleozoic-Mesozoic age. Carbonate rocks (marble) are also present locally. The phyllite and phyllonite are dark to silvery gray. The chert is mostly thin-bedded with phyllite partings. The Upper Paleozoic-Lower Mesozoic metasedimentary and metavolcanic rocks of the East Belt have been assigned to the Calaveras Complex by most investigators (Earhart, 1988). The Lower Paleozoic metamorphic rocks farther east have been assigned to the Shoo Fly Complex. More recently, some geologists have reinterpreted some assemblages along and immediately east of the Melones Fault Zone as separate Jurassic units (Schweickert and others, 1999). The metamorphic complexes are intruded in places by Mesozoic plutonic rocks.

Lode deposits of the East Belt consist of many individual gold-bearing quartz veins enclosed in metamorphic rocks of possible Jurassic age, metamorphic rocks of the Calaveras Complex, metamorphic rocks of the Shoo Fly complex, or in granitic rocks. Most of the veins trend northward and dip steeply. An east-west set of intersecting faults may be a controlling factor in controlling deposition of ore. Ore deposits of the East Belt are smaller and narrower than those of the Mother Lode, but commonly are more chemically complex, and richer in grade. Gold is usually associated with appreciable amounts of pyrite, chalcopyrite, pyrrhotite, galena, sphalerite, and arsenopyrite.

LOCAL GEOLOGY

The Chinese Camp District is underlain by a basement complex of ultramafic rock, metavolcanic rock, metasedimentary rock, and a small mass of plutonic rock. Small erosional remnants of Tertiary and Quaternary gravels are present on top of this complex and were the source of the placer gold in the district. The Tertiary gravels were deposited by the ancestral Tuolumne River.

Economic information about the deposit and operations

Operation type	Surface
Development status	Past Producer
Commodity type	Metallic
Deposit size	Small
Significant	Yes
Discovery year	1849

Mining district

District name	Chinese Camp District

Land status

Ownership category	Private
Area name	Tuolumne County Planning Department
Ownership category	BLM Administrative Area
Area name	Folsom Field Office

Comments on the workings information

This district was developed as a placer-mining center. Most of the early-day work during the gold rush was accomplished through small-scale surface methods, ground-sluicing, and hydraulicking. During the 1930?s there was some dragline dredging.

Comments on other economic factors

Clark (1970) estimated that the total output from placer mining in the district was about $2.5 million.

Comments on development

This district was settled in 1849 by Chinese placer miners. Peak mining activity probably took place in the 1850?s. Dragline dredging was attempted during the 1930?s, but apparently was found to be unprofitable. In one case the bedrock was too hard to permit saving more than a small fraction of the indicated gold content, most of which was evidently on or near bedrock.

Reference information

Bibliographic references

Deposit

Clark, W. B., 1970, Gold districts of California: California Division of Mines and Geology Bulletin 193, p. 37.
Deposit

Clark. W. B., and Lydon, P.A., 1962, Mines and mineral resources of Calaveras County, California: California Division of Mines and Geology County Report No. 2, p. 72-73.
Deposit

Earhart, R.L., 1988, Geologic setting of gold occurrences in the Big Canyon area, El Dorado County, California: U.S. Geological Survey Professional Paper 1576, 13 p.
Deposit

Higgins, C.T., 1997, Mineral land classification of a portionTurner, H.W. and Ransome, F.L., 1897, Geologic atlas of the United States, Sonora Folio, California: U.S. Geological Survey Folio 41, scale 1:125,000.
Deposit

of Tuolumne County, California, for precious metals, carbonate rock, and concrete-grade aggregate: California Division of Mines and Geology Open-File Report 97-09, 85 p.
Deposit

Julihn, C.E., and Horton, F.W., 1940, Mineral industries survey of the United States - Mines of the southern Mother Lode Region, Part II - Tuolumne and Mariposa counties: U.S. Bureau of Mines Bulletin 424, 179 p.
Deposit

Knopf, A., 1929, The Mother Lode system of California: U. S. Geological Survey Professional Paper 157, 88 p.
Deposit

Koschmann, A.H., and Bergendahl, M.H., 1968, Principal gold-producing districts of the United States: U. S. Geological Survey Professional Paper 610, 283 p.
Deposit

Logan, C.A., 1949, Mines and mineral resources of Tuolumne County, California: California Journal of Mines and Geology, v. 45, no. 1, p. 47-83.
Deposit

Schweickert, R.A., Hanson, R.E., and Girty, G.H., 1999, Accretionary tectonics of the Western Sierra Nevada Metamorphic Belt in Wagner, D.L. and Graham, S.A., editors, Geologic field trips in northern California: California Division of Mines and Geology Special Publication 119, p. 33-79.
Deposit

Turner, H.W. and Ransome, F.L., 1897, Geologic atlas of the United States, Sonora Folio, California: U.S. Geological Survey Folio 41, scale 1:125,000.
Deposit

Wagner, D.L., Bortugno, E.J., and McJunkin, R.D., 1990, Geologic map of the San Francisco-San Jose Quadrangle, California: California Department of Conservation, Division of Mines and Geology Regional Geologic Map Series, Map No. 5A, scale 1:250,000.
Deposit

Zimmerman, J.E., 1983, The geology and structural evolution of a portion of the Mother Lode Belt, Amador County, California: Unpublished M.S. thesis, University of Arizona, 138 p.

General comments

Subject category	Comment text
Deposit	The deposit consists of placer gold found in gravels deposited on top of an eroded basement surface. The gravels were deposited by streams that coursed through this area having eroded and carried gold from extensive quartz veins in the basement complex. Much of the placer gold recovered here was from extremely rich quartz-bearing gravels of Eocene age. Some gold was also mined from gravels of late Tertiary and Quaternary age as well as from the eroded basement surface that contained gold-bearing quartz veins in places.

Subject category

Comment text

Deposit

The deposit consists of placer gold found in gravels deposited on top of an eroded basement surface. The gravels were deposited by streams that coursed through this area having eroded and carried gold from extensive quartz veins in the basement complex. Much of the placer gold recovered here was from extremely rich quartz-bearing gravels of Eocene age. Some gold was also mined from gravels of late Tertiary and Quaternary age as well as from the eroded basement surface that contained gold-bearing quartz veins in places.

Reporter information

Type	Date	Name	Affiliation	Comment
Reporter	14-AUG-2006	Higgins, Chris T.	California Geological Survey CGS (Formerly CDMG)
Editor	01-SEP-2007	Schruben, Paul G.	U.S. Geological Survey	Converted from S&A FileMaker format to Oracle. Edit checks on rocks, units, and ages with Geolex search, and other fields.

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

Maps centered on this site

Authoritative California resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.