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Nowell-Otterson Prospect, Admiralty Mining District, Hoonah-Angoon Census Area, Alaska, USAi
Regional Level Types
Nowell-Otterson ProspectProspect
Admiralty Mining DistrictMining District
Hoonah-Angoon Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
58° 12' 35'' North , 134° 51' 18'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Juneau32,756 (2017)27.4km
Tenakee Springs133 (2017)52.3km
Mindat Locality ID:
199189
Long-form identifier:
mindat:1:2:199189:8
GUID (UUID V4):
0


Location: The Nowell-Otterson prospect is at an elevation of approximately 2500 feet on Mansfield Peninsula, 2.25 miles southeast of Funter Bay, 1.5 miles northwest of Snowy Mountain, and 1 mile south of Mount Robert Barron. It is in the SW1/4SW1/4 section 19, T. 42 S., R. 65 E. of the Copper River Meridian. The location is accurate. The Alaska Dano (JU236) and the Nowell-Patterson prospect are in the same block of patented mining claims.
Geology: This deposit was discovered prior to 1898 (Wells and others, 1986). It consists of multiple quartz veins in mica schist and chlorite schist near a granitic intrusive (Cobb, 1978 [OFR 78-374]). The veins strike N 20 W. and dip NE, parallel to the strike of the schistose host rocks. The veins can be traced discontinuously northwest to the Alaska Dano Mine (JU235). One vein is 15 to 25 feet thick and has been traced for 2,300 feet. It consists of quartz and calcite, with pyrite and pyrrhotite, and minor galena, specular hematite, and native gold. Another vein, 30 inches thick, consists of white quartz, pyrite, specular hematite, and minor chalcopyrite, galena, and copper oxides. It is crosscut by a calcite vein. The prospect is developed by 2 shafts, an unknown amount of drifts, and some open cuts (Wells and others, 1986). The prospect is included with the Alaska Dano and War Horse deposits in some reports (Cobb, 1978). The rocks in the general area are mainly Ordovician and Devonian to Triassic clastic units, mafic-intermediate volcanic rocks, and subordinate limestone. The bedded rocks are intruded and locally metamorphosed by Cretaceous granodiorite (Gehrels and Berg, 1994).
Workings: The prospect is developed by 2 shafts,an unknown amount of drifts, and some open cuts (Wells and others, 1986).
Alteration: Local oxidation of copper and iron minerals.

Commodities (Major) - Ag, Au, Cu, Pb, Zn
Development Status: Undetermined.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


9 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘGold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
ⓘSphalerite2.CB.05aZnS
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘGalena2.CD.10PbS
ⓘPyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
ⓘHematite4.CB.05Fe2O3
ⓘQuartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3

List of minerals for each chemical element

CCarbon
Cⓘ CalciteCaCO3
OOxygen
Oⓘ CalciteCaCO3
Oⓘ HematiteFe2O3
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2
SSulfur
Sⓘ ChalcopyriteCuFeS2
Sⓘ GalenaPbS
Sⓘ PyriteFeS2
Sⓘ PyrrhotiteFe1-xS
Sⓘ SphaleriteZnS
CaCalcium
Caⓘ CalciteCaCO3
FeIron
Feⓘ ChalcopyriteCuFeS2
Feⓘ HematiteFe2O3
Feⓘ PyriteFeS2
Feⓘ PyrrhotiteFe1-xS
CuCopper
Cuⓘ ChalcopyriteCuFeS2
ZnZinc
Znⓘ SphaleriteZnS
AuGold
Auⓘ GoldAu
PbLead
Pbⓘ GalenaPbS

Other Databases

Link to USGS - Alaska:JU236

Other Regions, Features and Areas containing this locality


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