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Alps mine, Treasure Hill, Pioche, Pioche Mining District, Lincoln County, Nevada, USAi
Regional Level Types
Alps mineMine
Treasure HillHill
PiocheTown
Pioche Mining DistrictMining District
Lincoln CountyCounty
NevadaState
USACountry

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Latitude & Longitude (WGS84):
37° 54' 56'' North , 114° 25' 48'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Pioche1,002 (2011)2.5km
Panaca963 (2011)14.4km
Caliente1,109 (2017)34.2km
Mindat Locality ID:
57669
Long-form identifier:
mindat:1:2:57669:4
GUID (UUID V4):
0


Structure: Highland Thrust Plate, Major Nw Trending Normal Faults Thrust Fault And Faults Cutting Off Ore And Yuba Dike.

Alteration: Sericitic Alteration Of Yuba Dike.

Commodity: Unusually high gold content for pioche ore

Deposit: Ore body faulted off at about 300 ft depth. Quartzite highly brecciated and cemented by silica stained with Mn-Fe oxides. Phyllitic shale observed on dump along with abundant gossan. Galena occurs As clots and stringers in quartz vein which cuts white quartzite along with minor pyrite. Copper oxides and crystalline jarosite along with mustard yellow oxides (sb oxides?) coat fractures and breccia fragments. Yuba dike extends to general vicinity of the mine, where it has been intersected at depth. On the east, the vein has been cut off by a fault that strikes n55w, dip 55sw. 3 veins present, reported to contain "5-10 oz Ag to each unit of Pb". 2 of the veins coincide with the hanging wall and footwall of the yuba dike, while the so-called "middle vein" is along a set of fractures paralleling the strike of and wholly contained within the dike.

Deposit type: Polymetallic veins

Development: Alps silver mining co owned the old floral mill. No activity at time of examination in 1983, but tailings had been milled recently and one shaft was being used As a landfill. One of the oldest mines in the district, the alps shaft had already been sunk to a depth of 115 ft by 1871.

Geology: Ore occurs in fissure vein and brecciated zones of pb carbonate in a quartz gangue, which is usually white. The main vein is 1 to 4 feet thick. At depth the vein terminates against shale. Host rocks are white to grey banded quartzite dipping s W up to 40, phyllitic shales. Granite porphyry dike (yuba dike) 40 ft wide, dip 70s.

Rock formation(s): Yuba Dike; Prospect Mountain Quartzite


Ore(s): Faulting. Extension Of Yuba Dike Intersecting With A Cross-Fissure; Brecciation.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity 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!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Jarosite7.BC.10KFe3+3(SO4)2(OH)6

List of minerals for each chemical element

HHydrogen
H JarositeKFe33+(SO4)2(OH)6
OOxygen
O JarositeKFe33+(SO4)2(OH)6
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S GalenaPbS
S JarositeKFe33+(SO4)2(OH)6
S PyriteFeS2
KPotassium
K JarositeKFe33+(SO4)2(OH)6
FeIron
Fe JarositeKFe33+(SO4)2(OH)6
Fe PyriteFeS2
AuGold
Au Native GoldAu
PbLead
Pb GalenaPbS

Other Databases

Link to USGS MRDS:10037328

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