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Gulch Creek No. 2 Occurrence, Hope Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Gulch Creek No. 2 OccurrenceOccurrence
Hope Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 46' 34'' North , 149° 19' 55'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Girdwood2,250 (2017)20.5km
Hope192 (2017)22.9km
Moose Pass219 (2014)32.1km
Cooper Landing289 (2017)41.7km
Primrose111 (2006)44.2km
Mindat Locality ID:
197849
Long-form identifier:
mindat:1:2:197849:3
GUID (UUID V4):
0


Location: This occurrence is located in the NE1/4 section 19, T. 8 N., R. 1 E., of the Seward Meridian. It is situated at the head of a small cirque valley on the south side of Gulch Creek, at elevations between 3,200 and 3,350 feet. This is location S-283 of Jansons and others (1984). The location is accurate to within a quarter of a mile.
Geology: The Gulch Creek No. 2 occurrence consists of at least two subparallel quartz-carbonate veins that strike N55-60E and dip 45-50SE. The veins average 1.5 feet thick and are locally as much as 4 feet wide. They can be traced for 100 to 200 feet along strike. The quartz has a well-developed ribbon structure, is highly fractured, and contains arsenopyrite and minor pyrite along the contact with the wallrock. Slickensides along the hanging wall of one vein are horizontal and indicate a right-lateral movement (Hoekzema and Sherman, 1983). The Valdez Group (Late Cretaceous age) host rock (Nelson and others, 1985) is mostly highly fractured slate and metasiltstone having foliation that strikes N30-35E and dips 55-60SE (Hoekzema and Sherman, 1983). Five samples were collected by the U.S. Bureau of Mines in 1982.; they assayed trace amounts of gold and as much as 0.01 ounce of silver per ton (Jansons and others, 1984).
Workings: No workings or improvements are present. The occurrence was discovered by the U.S. Bureau of Mines in 1982; at that time they examined and sampled two veins (Hoekzema and Sherman, 1983). The five samples they collected assayed trace amounts of gold and as much as 0.01 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.

Commodities (Major) - 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
Pyrite2.EB.05aFeS2
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 PyriteFeS2
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ArsenopyriteFeAsS
Fe PyriteFeS2
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au Native GoldAu

Other Databases

Link to USGS - Alaska:SR032

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.

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