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Eagle-Shawmut Mine (Belmont-Shawmut Mine), Hog Mountain, Jacksonville Mining District, Tuolumne County, California, USAi
Regional Level Types
Eagle-Shawmut Mine (Belmont-Shawmut Mine)Mine
Hog MountainMountain
Jacksonville Mining DistrictMining District
Tuolumne CountyCounty
CaliforniaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
37° 52' 2'' North , 120° 23' 44'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Chinese Camp126 (2011)3.3km
Jamestown3,433 (2011)9.9km
East Sonora2,266 (2011)12.6km
Sonora4,818 (2017)13.0km
Groveland601 (2011)14.7km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Calaveras Gem & Mineral SocietyAngels Camp, California26km
Mindat Locality ID:
97703
Long-form identifier:
mindat:1:2:97703:3
GUID (UUID V4):
13cfdef5-dfbf-4470-b2f2-269b372b31e3


A former lode Au mine located in sec. 11, T1S, R14E, MDM, 4.1 km (2.5 miles WSW of Hog Mountain (coordinats of record) (on Wood Creek, 2 miles NW of Jacksonville). Operated by the Belmont-Shawmut Mining Co. (1923-1928). MRDS database stated accuracy for this location is 10 meters. Not much work done before 1896 when the Eagle and Shawmut claims were joined together. References include report on each mine separately.

Mineralization is hosted in slate, amphibolite and schist. The slate is interbedded with thin-layered sandstone averaging 2 inches. Lenses of limestone 2 to 3 feet thick occur above volcanic rocks and thinner lenses of conglomerate occur in slate below the volcanics. A narrow belt of pyroxenite or hornblendite, or an allied hornblende-pyroxene peridotite exists between green-chlorite schist and black slate. For a more complete geologic description see Knopf (1929). Local alteration involves a pyroxenite intrusive which has been sheared and altered to multiform chlorite schist and subsequently ankerized and silicified. Chlorite schist sometimes resembles serpentine schist due to the lusterous green; in places this rock has a pseudomorphic texture much like serpentinized peridotite but the phenocrysts instead of being bastite are chlorite embedded in a fine-grained chlorite matrix. Local rocks include Jurassic marine rocks, unit 1 (Western Sierra Nevada and Western Klamath Mountains) and/or Undivided pre-Cenozoic metavolcanic rocks, unit 2 (undivided).

Workings include underground openings with an overall depth of 914.4 meters. A crosscut adit 1,100 feet long through the footwall to the lode connects with an inclined shaft 2,163 feet, with 19 levels at various intervals.

Sulfides comprise as much as 15% of total ore.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2

List of minerals for each chemical element

CCarbon
C AnkeriteCa(Fe2+,Mg)(CO3)2
OOxygen
O AnkeriteCa(Fe2+,Mg)(CO3)2
O QuartzSiO2
MgMagnesium
Mg AnkeriteCa(Fe2+,Mg)(CO3)2
SiSilicon
Si QuartzSiO2
SSulfur
S PyriteFeS2
CaCalcium
Ca AnkeriteCa(Fe2+,Mg)(CO3)2
FeIron
Fe AnkeriteCa(Fe2+,Mg)(CO3)2
Fe PyriteFeS2
AuGold
Au GoldAu

Other Databases

Link to USGS MRDS:10077877

Other Regions, Features and Areas containing this locality

North America PlateTectonic Plate
USA

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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