Porcupine Creek Occurrence, Hope Mining District, Kenai Peninsula Borough, Alaska, USAi
| Regional Level Types | |
|---|---|
| Porcupine Creek Occurrence | Occurrence |
| Hope Mining District | Mining District |
| Kenai Peninsula Borough | Borough |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
60° 18' 7'' North , 149° 26' 49'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Primrose | 111 (2006) | 10.9km |
| Bear Creek | 1,956 (2017) | 15.6km |
| Moose Pass | 219 (2014) | 21.1km |
| Seward | 2,790 (2017) | 22.0km |
| Cooper Landing | 289 (2017) | 29.5km |
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 ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
5 valid minerals.
Detailed Mineral List:
| ⓘ Arsenopyrite Formula: FeAsS |
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Galena Formula: PbS |
| ⓘ Native Gold Formula: Au |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Quartz | SiO2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Galena | PbS |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Arsenopyrite | FeAsS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Databases
| Link to USGS - Alaska: | SR190 |
|---|
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