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Octaroon Mine, Coyote Canyon, Tijeras Canyon Mining District, Bernalillo County, New Mexico, USAi
Regional Level Types
Octaroon MineGroup of Mines
Coyote CanyonCanyon
Tijeras Canyon Mining DistrictMining District
Bernalillo CountyCounty
New MexicoState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
34° 56' 43'' North , 106° 26' 34'' West
Latitude & Longitude (decimal):
Type:
Group of Mines
Nearest Settlements:
PlacePopulationDistance
Ponderosa Pine1,195 (2011)11.4km
Cedro430 (2011)11.8km
Carnuel1,232 (2011)13.2km
Tijeras541 (2011)15.9km
Meadow Lake4,708 (2011)18.4km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Albuquerque Gem & Mineral ClubAlbuquerque, New Mexico24km
Mindat Locality ID:
241083
Long-form identifier:
mindat:1:2:241083:1
GUID (UUID V4):
d55adf08-355b-4284-b80c-0e551d9e831b


The Galena King/Octoroon/Frustration mines were mined for lead. The Octoroon mine has two adits, with the northern one collapsed. The southern adit has a winze as well.
[Ray De Mark 2012]
The barite from the Octaroon mine is in thin blades while the barite from the Galena King has coarse, opaque blades that are often coated with drusy fluorite or in some case "hooded" by drusy fluorite. Barite from the Frustration mine is not noteworthy and much less common than at the Galena King or Octaroon.

Both the Galena King and the Octoroon mines are in Bernalillo Co. (as well as the Frustration mine). The Octoroon mine is about a half mile west of the Galena King and somewhat lower in elevation. The minerals at the Octaroon are virtually the same as at the Galena King (fluorite, barite, galena, quartz w/minor chalcopyrite and malachite). The barite occurs in bladed, usually white xtals and is more noteworthy than the fluorite. The fluorite is mostly in stepped octahedrons and usually a light purple to blue.

The mines were mapped in 1923 by Fayette Jones (maps held by the NM Bureau of Geology and Mineral Resources). These maps show all the adits and shafts. The mineralized veins are all almost vertical and occur in pre-Cambrian granite (gneiss).
[Raymond De Mark 2012]

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Galena2.CD.10PbS
Group 3 - Halides
β“˜Fluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Baryte7.AD.35BaSO4

List of minerals for each chemical element

HHydrogen
Hβ“˜ MalachiteCu2(CO3)(OH)2
CCarbon
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ BaryteBaSO4
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ QuartzSiO2
FFluorine
Fβ“˜ FluoriteCaF2
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ BaryteBaSO4
Sβ“˜ GalenaPbS
CaCalcium
Caβ“˜ FluoriteCaF2
CuCopper
Cuβ“˜ MalachiteCu2(CO3)(OH)2
BaBarium
Baβ“˜ BaryteBaSO4
PbLead
Pbβ“˜ GalenaPbS

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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