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Thorpe Mine, Quiggs Mountain, Mountain Ranch Mining District, East Belt, Calaveras County, California, USAi
Regional Level Types
Thorpe MineMine
Quiggs MountainMountain
Mountain Ranch Mining DistrictMining District
East Belt- not defined -
Calaveras CountyCounty
CaliforniaState
USACountry

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Latitude & Longitude (WGS84):
38° 12' 29'' North , 120° 37' 24'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
San Andreas2,783 (2011)5.2km
Mountain Ranch1,628 (2011)7.6km
Mokelumne Hill646 (2011)12.6km
Murphys2,213 (2015)16.2km
Angels Camp2,677 (2012)17.2km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Calaveras Gem & Mineral SocietyAngels Camp, California17km
Amador County Gem & Mineral SocietySutter Creek, California26km
Mindat Locality ID:
75999
Long-form identifier:
mindat:1:2:75999:6
GUID (UUID V4):
7e24d63f-0f57-4a1d-8c80-92bac14ce66d


A former lode Au mine located in the SWΒΌ (estimated) sec. 11, T3N, R11E, MDM, 2.5 km (1.6 miles) SSW of Quiggs Mountain (coordinates of record), just W of highway 49 (6 miles S of Mokelumne Hill [town]). Operated in a small way prior to 1894. MRDS database stated accuracy for this location is 100 meters.

Mineralization is a vein deposit hosted in amphibolite, schist, slate and phyllite. The ore body strikes N60W and dips 53NE at a thickness of 15.24 meters and is comprised of a zone of parallel quartz veins and stringers in amphibolite and chlorite schist. Small amounts of talc and sericite schist are adjacent. Phyllite and slate occur to the W. The thickness of the 3 principal veins average 15 feet but reach 50 feet. The veins are mostly in schist. Ore occurs mostly at the intersection of main and minor fissuring. Levels show fair values. Local rocks include Mesozoic volcanic rocks, unit 2 (Western Sierra Foothills and Western Klamath Mountains) and/or Paleozoic marine rocks, undivided, unit 4 (Western Sierra Nevada).

Workings include underground openings with an overall depth of 194.16 meters, and comprised of a 700 foot main shaft inclined at 55 degrees (now flooded). Stoping occurred on the 300, 400 and 500 foot levels. There is also a 600 foot level.

Production data are found in: Clark, Wm. B. & P.A. Lydon (1962).

Produced a few thousand dollars (period values) in 1895.

Analytical data results: 3% sulfides.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


7 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
β“˜Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
Group 9 - Silicates
β“˜Talc9.EC.05Mg3Si4O10(OH)2
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
β“˜'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ TalcMg3Si4O10(OH)2
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CCarbon
Cβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Cβ“˜ CalciteCaCO3
OOxygen
Oβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Oβ“˜ CalciteCaCO3
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ TalcMg3Si4O10(OH)2
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
MgMagnesium
Mgβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Mgβ“˜ TalcMg3Si4O10(OH)2
AlAluminium
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ QuartzSiO2
Siβ“˜ TalcMg3Si4O10(OH)2
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
Sβ“˜ PyriteFeS2
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Caβ“˜ CalciteCaCO3
FeIron
Feβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Feβ“˜ PyriteFeS2
AuGold
Auβ“˜ GoldAu

Other Databases

Link to USGS MRDS:10028769

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References

 
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