Morning Star Mine (Curtz Mine; Ardis Mine), Mogul Peak, Monitor - Mogul Mining District, Alpine County, California, USAi
| Regional Level Types | |
|---|---|
| Morning Star Mine (Curtz Mine; Ardis Mine) | Mine |
| Mogul Peak | Peak |
| Monitor - Mogul Mining District | Mining District |
| Alpine County | County |
| California | State |
| USA | Country |
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Latitude & Longitude (WGS84):
38° 40' 58'' North , 119° 41' 57'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Markleeville | 210 (2014) | 7.3km |
| Topaz Lake | 157 (2011) | 13.5km |
| Alpine Village | 114 (2011) | 14.4km |
| Mesa Vista | 200 (2011) | 16.2km |
| Topaz Ranch Estates | 1,501 (2017) | 18.2km |
A former lode Au-Cu-Ag-Sb-Pb-Zn-As-baryte mine located in the W½ sec. 29, T10N, R21E, MDM, 1.7 km (5,500 feet) ESE of Mogul Peak and 2.0 km (6,400 feet) N of Loope, along Mogul Gulch (3 miles NW from Heenan Lake), on National Forest land. MRDS database stated accuracy for this location is 100 meters.
Mineralization is hosted in Pliocene andesitic rhyolite. Geologic structures involve a shear zone. Alteration is local (silicification). This deposit is on the E side of the major alteration/silicification of the district. The shear zone appears to trend SW through the Curtz & Georgiana Mines, and then SE along the S side of Monitor Canyon near the Zaca mill. The mine dump has white, silicified rock that contains mostly fine- to medium-grained minerals. The silicified hilltop stands out from surrounding unaltered andesite. The silicified rock is iron oxide-stained in places. This mine resembles other district producers except that enargite is more abundant. Enargite (or other copper-arsenic-antimony sulfosalts) is the most important copper ore mineral (Burchard 1883). A body of enargite mixed with pyrite was found in the late 19th century, measuring 10 to 15 feet thick and 20 to 30 feet long. Local rocks include Tertiary pyroclastic and volcanic mudflow deposits, unit 9 (Cascade Range).
From Wachter (1971): Jasperoid outcrop is mostly quartz and has silver and gold with high trace elements. Hydrothermal alteration at the Morningstar deposit was caused by fluids with a low K+/H+ ratio (orthoclase is almost absent). The "clay" associated with enargite is quartz, kaolinite, and pyrite. The "clay" associated with massive pyrite is quartz with lesser sericite and dickite. Sericitic alteration and quartz-jasperoid present at Morningstar and Mogul Peak.
Also from Wachter (1971): A sample of enargite yielded 16% copper, 50 ounces per ton silver, and 0.5 ounce per ton gold. Similar material showed blebs of an unknown silver mineral in enargite, and possible cylindrite was intergrown with enargite. A sample of porous pyrite (with no other visible sulfides) yielded 0.2% copper, 5 ounces per ton silver, and 0.08 ounce per ton gold.
Workings include underground openings. A 1,200 foot main adit, trending SSE, is known as the 148 foot level. A 480 foot deep shaft connected 922 feetN from the portal. There are also 220, 280 and 480 foot levels. Crosscuts extend to the ore zone. Also stopes and winzes. The main adit & shaft were still open in 1971. Workings of the Georgiana & Curtz Mines were for a time driven for ore bodies in the same zone.
Production data are found in: Clark (1977).
Some enargite ore (carrying $400 (period values) per ton in Cu, Au & Ag) was shipped as far as Swansea, Wales, for smelting. The mine produced fairly steadily during the period 1863 - 1904 on a fairly large scale. Minor exploration was done in 1951, 1952 & 1957.
1882: Over a six month and 16 day period, an average of 3.5 tons of ore per day was processed in the Exchequer mill with the Hunt, Douglass, and Stewart Process. The total output for this period was 70,895 pounds of copper and $18,172 (period values) of Au & Ag.
1901: 22 tons of ore yielded 17% copper, $32.00 (period values) in Au, and 49 ounces of Ag per ton.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Acanthite Formula: Ag2S |
| ⓘ Alunite Formula: KAl3(SO4)2(OH)6 |
| ⓘ Arsenopyrite Formula: FeAsS Description: Well-formed crystals. References: |
| ⓘ Baryte Formula: BaSO4 Description: A gangue mineral. |
| ⓘ Bismuthinite Formula: Bi2S3 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Emplectite Formula: CuBiS2 |
| ⓘ Enargite Formula: Cu3AsS4 Description: Principal Cu ore mineral here. |
| ⓘ Famatinite Formula: Cu3SbS4 |
| ⓘ 'Freibergite Subgroup' Formula: (Ag6,[Ag6]4+)(Cu4 C2+2)Sb4S12S0-1 |
| ⓘ Galena Formula: PbS |
| ⓘ Galena var. Silver-bearing Galena Formula: PbS with Ag |
| ⓘ Goldfieldite Formula: (Cu4◻2)(Cu4Cu+2)Te4S12S |
| ⓘ Luzonite Formula: Cu3AsS4 References: |
| ⓘ Native Gold Formula: Au |
| ⓘ Native Sulphur Formula: S8 |
| ⓘ Polybasite Formula: [Ag6Sb2S7][Ag9CuS4] Description: Occurs as microscopic crystals. References: |
| ⓘ Pyrargyrite Formula: Ag3SbS3 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Realgar Formula: As4S4 |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ Stephanite Formula: Ag5SbS4 References: |
| ⓘ Stromeyerite Formula: AgCuS |
| ⓘ 'Tennantite Subgroup' Formula: Cu6(Cu4C2+2)As4S12S |
| ⓘ 'Tetrahedrite Subgroup' Formula: Cu6(Cu4C2+2)Sb4S12S Description: An important ore here. |
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| ⓘ | Native Sulphur | 1.CC.05 | S8 |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | Stromeyerite | 2.BA.40 | AgCuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | var. Silver-bearing Galena | 2.CD.10 | PbS with Ag |
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | Realgar | 2.FA.15a | As4S4 |
| ⓘ | Pyrargyrite | 2.GA.05 | Ag3SbS3 |
| ⓘ | 'Freibergite Subgroup' | 2.GB.05 | (Ag6,[Ag6]4+)(Cu4 C2+2)Sb4S12S0-1 |
| ⓘ | Goldfieldite | 2.GB.05 | (Cu4◻2)(Cu4Cu+2)Te4S12S |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | Stephanite | 2.GB.10 | Ag5SbS4 |
| ⓘ | Polybasite | 2.GB.15 | [Ag6Sb2S7][Ag9CuS4] |
| ⓘ | Emplectite | 2.HA.05 | CuBiS2 |
| ⓘ | Enargite | 2.KA.05 | Cu3AsS4 |
| ⓘ | Famatinite | 2.KA.10 | Cu3SbS4 |
| ⓘ | Luzonite | 2.KA.10 | Cu3AsS4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| ⓘ | Alunite | 7.BC.10 | KAl3(SO4)2(OH)6 |
List of minerals for each chemical element
Other Databases
| Link to USGS MRDS: | 10006814 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Northern Basin and RangeWide Rift
- Shoofly-Olds Ferry DomainDomain
USA
- Sierra NevadaMountain Range
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References
(n.d.) Minerals Availability System (MAS), U.S. Bureau of Mines.file ID #0060030029
Aubury, Lewis E. (1905) The Copper Resources of California. Bulletin 23. California State Mining Bureau p.199
[3](1908, September) The Copper Resources of California. Bulletin 50. California State Mining Bureaup.246
Harcourt, G. Alan (1937) The distinction between enargite and famatinite (luzonite) American Mineralogist, 22 (5) 517-525 p.521
Bramel, Hadley R., Heyl, George R., Cox, Manning W., Ransome, Alfred L., Eric, John H., Wyant, Donald G. (1948) Copper in California. Bulletin 144. California State Mining Bureau p.213




Morning Star Mine, Mogul Peak, Monitor - Mogul Mining District, Alpine County, California, USA