Marcus Mine, Potosi Mining District, Osgood Mountains, Humboldt County, Nevada, USAi
| Regional Level Types | |
|---|---|
| Marcus Mine | Mine |
| Potosi Mining District | Mining District |
| Osgood Mountains | Mountain Range |
| Humboldt County | County |
| Nevada | State |
| USA | Country |
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Latitude & Longitude (WGS84):
41° 9' 20'' North , 117° 17' 58'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Golconda | 214 (2011) | 27.6km |
| Winnemucca | 7,887 (2017) | 41.8km |
| Paradise Valley | 109 (2011) | 42.4km |
| Orovada | 155 (2011) | 61.3km |
Other/historical names associated with this locality:
Markus Mine; Harden's Lease
Sec 24 T38N R42E. Tactite
Deposit: The property was explored prior to 1955, but no mining was done until road had been built to it from the granite creek mine in 1955, when open-pit mining began. It consists of five unpatented claims. Workings include 2 short adits, trenches, and open cuts. 300-350 tons of 1.7% wo3 ore and 1000 to 1300 ton S of 0.5% wo3 ore were estimated to be present in 1946, As well As 6000 to 12,000 tons of 0.3% wo3 or less ore possible ; info.src : 1 pub lit; 2 unpub rept the deposit is on the west side of the south part of the granodiorite stock near the crest of the range. The contact zone between the stock and the sedimentary rocks is highly irregular. Slide rock covers much of the surface in the vicinity of the mine and exposures are poor. Small and discontinuous tactite bodies occur where the thin limestone beds, in argillite and hornfels, are truncated by the granodiorite stock or by irregular apophyses. The tactite bodies mined were from a Few feet to 25 feet wide and probably averaged about 20 ft. The tungsten content ranged from 0.1 % wo3 to 3.34 % but probably averaged about 0.5 % wo3. Workings extend along 1200 ft strike
Deposit type: W skarn
Development: 300-350 tons of 1.7% wo3 ore and 1000-1300 tons of 0.5% wo3 ore estimated present in 1946, As well As 6000 to 12,000 tons of 0.3% wo3 ore possible. In 1943, the property was owned by john etchert, jr., and w. M. Pettit, and leased to john h. Harden of winnemucca. Workings consisted of numerous trenches, open cuts and 2 Short adits, but access to the property was difficult. In 1955, the property was acquired by getchell mines and a road was constructed up granite creek from the granite creek mine, replac-ing the 2.5 to 3 miles of rough trail. Open-pit mining in 1955 and 1956 yielded 21300 tons of ore that were trucked to the getchell mill. 5 unpatented claims.
Geology: Main tactite body 2 to 10 ft. Wide and over 75 ft. Long along a very irregular contact. There are 4 tactite bodies
Rock formation(s): Osgood Mtns. Stock
Preble Formation
Ore(s): Tactite At Granodiorite/Limestone Contact
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
5 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Scheelite Formula: Ca(WO4) |
| ⓘ Vesuvianite Formula: Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
| Group 9 - Silicates | |||
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Vesuvianite | 9.BG.35 | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| Unclassified | |||
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Scheelite | Ca(WO4) |
| O | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| Mg | Magnesium | |
| Mg | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| Al | Aluminium | |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| Si | Silicon | |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Scheelite | Ca(WO4) |
| Ca | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| Fe | Iron | |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
| W | Tungsten | |
| W | ⓘ Scheelite | Ca(WO4) |
Other Databases
| Link to USGS MRDS: | 10045083 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Northern Basin and RangeWide Rift
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