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Porcupine Creek Occurrence, Hope Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Porcupine Creek OccurrenceOccurrence
Hope Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 18' 7'' North , 149° 26' 49'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Primrose111 (2006)10.9km
Bear Creek1,956 (2017)15.6km
Moose Pass219 (2014)21.1km
Seward2,790 (2017)22.0km
Cooper Landing289 (2017)29.5km
Mindat Locality ID:
199459
Long-form identifier:
mindat:1:2:199459:2
GUID (UUID V4):
0


Location: The occurrence is located a mile west of Porcupine Creek and three-quarters of a mile southeast of peak 3722. It is in the SE1/4 section 33, T. 3 N., R. 1 W., of the Seward Meridian, at an elevation of 3,000 feet. This is location S-212 of Jansons and others (1984). This location is accurate to within a quarter of a mile.
Geology: Mineralization consists of several quartz veins containing minor amounts of sulfide minerals. One vein in a small gulch is 1 to 3 feet wide; it contains calcite and minor arsenopyrite (Hoekzema and Sherman, 1983). The host rock is iron-stained slate on the footwall; foliation strikes N10E and dips 85E. The hanging wall is metasandstone. Several 1- to 3-inch-thick veins are located 200 to 300 feet south and 200 feet above the large vein. These smaller veins are hosted in graywacke and strike N75W and dip 85N. They contain considerable arsenopyrite and minor galena. The host rock is slate and graywacke of the Valdez Group of Late Cretaceous age (Nelson and others, 1985). Three samples assayed trace amounts of gold and as much as 0.2 ounce of silver per ton (Jansons and others, 1984).
Workings: There are no workings or improvements described in the literature. Three samples assayed trace amounts of gold and as much as 0.2 ounce of silver per ton (Jansons and others, 1984).
Age: Cretaceous or younger; the veins cut rocks of the Valdez Group of Late Cretaceous age.
Alteration: The slate in the footwall is iron-stained.

Commodities (Major) - Ag?, Au
Development Status: None
Deposit Model: Low-sulfide Au-quartz veins (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
Galena2.CD.10PbS
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
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 QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ArsenopyriteFeAsS
S GalenaPbS
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ArsenopyriteFeAsS
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au Native GoldAu
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:SR190

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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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