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Unnamed Prospect (ARDF - SV021; in Port Dick), Homer Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Unnamed Prospect (ARDF - SV021; in Port Dick)- not defined -
Homer Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
59° 18' 46'' North , 151° 21' 25'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Seldovia277 (2017)24.4km
Seldovia Village165 (2011)24.8km
Port Graham177 (2011)27.1km
Homer5,515 (2017)38.2km
Kachemak City472 (2013)39.8km
Mindat Locality ID:
202452
Long-form identifier:
mindat:1:2:202452:6
GUID (UUID V4):
0


This prospect is within Kachemak Bay State Wilderness Park; the area is withdrawn from mineral entry.
Location: The prospects are about a mile and a quarter west of the head of Port Dick in the NW 1/4 section 17, T.10 S., R. 12 W., of the Seward Meridian, and the NE 1/4 of section 18, T.10 S., R. 12 W., of the Seward Meridian. The lower adit is about 200 feet above sea level, and the upper adit is about 500 feet above sea level. This is Cobb's (1972, MF-397) location 14. This location is accurate within a quarter of a mile.
Geology: The country rock at the head of the West Arm of Port Dick is hornfelsed graywacke and greenstones of the Cretaceous Valdez Group that have been intruded by fine-grained biotite granite dikes of Tertiary age (MacKevett and Holloway, 1978). The quartz veins are nearly vertical and cut both the granite dikes and the graywacke. The lower prospect is at about 200 feet of elevation where an adit 140 feet long was driven on a vein that strikes N54W and dips 75 to 85N. The vein ranges from 6 to 20 inches in width and averages 15 inches thick. The vein consists of quartz with segregations of arsenopyrite and pyrite that give the vein a banded appearance. The upper vein at an elevation of about 500 feet is about 500 feet to the south. It is about 24 inches thick. An adit 310 feet long has been driven N69W along strike on the vein. The upper vein is similar to the lower vein and contains traces of sphalerite and small fractures filled with calcite. The wall rock is a fine-grained granite (Brooks, 1909).
Workings: Several hundred feet of tunnels were driven in 1899, and 1904 through 1907 by the Alaska Commercial Company. A grab sample provided to Brooks (1909) assayed at 0.123 ounces of gold and 1.32 ounces of silver per ton. There is no reported production from this location.
Age: Tertiary; veins cut Tertiary granite dikes.
Alteration: None reported.
Production: None reported.
Reserves: None reported.

Commodities (Major) - Au; (Minor) - Ag, Cu, Zn
Development Status: None
Deposit Model: Low-sulfide, Au-quartz vein (Cox and Singer, 1986; model 36a)

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


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
ⓘSphalerite2.CB.05aZnS
ⓘPyrite2.EB.05aFeS2
ⓘArsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2
SSulfur
Sⓘ ArsenopyriteFeAsS
Sⓘ PyriteFeS2
Sⓘ SphaleriteZnS
FeIron
Feⓘ ArsenopyriteFeAsS
Feⓘ PyriteFeS2
ZnZinc
Znⓘ SphaleriteZnS
AsArsenic
Asⓘ ArsenopyriteFeAsS
AuGold
Auⓘ Native GoldAu

Other Databases

Link to USGS - Alaska:SV021

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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