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Timberline Prospects, Valdez Creek Mining District, Matanuska-Susitna Borough, Alaska, USAi
Regional Level Types
Timberline ProspectsGroup of Prospects
Valdez Creek Mining DistrictMining District
Matanuska-Susitna BoroughBorough
AlaskaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
63° 11' 16'' North , 147° 24' 3'' West
Latitude & Longitude (decimal):
Type:
Group of Prospects
KΓΆppen climate type:
Mindat Locality ID:
200363
Long-form identifier:
mindat:1:2:200363:7
GUID (UUID V4):
afb536e1-7ec8-4984-9241-a8ea836d685f


This was one of the very few lode gold producers in the Valdez Creek drainage.
Location: The site represents several prospects at an elevation of about 3,950 feet on the west slope of the ridge between Timberline Creek and Valdez Creek. The map site is in the N1/2 of sec. 17, T. 20 S., R. 2 E., of the Fairbanks Meridian. The location is accurate to within 1,000 feet. These prospects are shown as Sites 6 through 10 on Plate I of Smith, 1981.
Geology: The country rock in the area of this site is spotted phyllite, cut by CHLORITIZED DIORITE of probable Cretaceous age. The deposit consists of five veins in shear zones in altered diorite. The largest vein, the Big Caribou, has been traced for 1,000 feet; it is up to 8 feet wide, and contains kidneys and lenses of quartz, arsenopyrite, pyrite, pyrrhotite, and chalcopyrite. Other veins include the Big Water Hole, Freda G., Valdez Creek 6, and Little Caribou. Veins comprise quartz bands up to 2 feet wide. Some of the sulfides also are disseminated in the diorite. The veins appear to be localized in a conjugate fracture system associated with east-trending fault zones. Samples of the veins contain up to 0.33 ounce of gold per ton (Smith, 1981).
Workings: Surface exploration consists of trenches and pits along the traces of the veins. A short adit was driven which encountered the down-dip extension of the Big Caribou and Little Caribou vein systems. Samples of the veins contain up to 0.33 ounce of gold per ton (Smith, 1981).
Age: Probably Cretaceous or younger.
Alteration: The quartz veins are associated with chloritization of the adjacent diorite.
Production: A small mill was installed in about 1934; it consisted of a jaw crusher, ball mill, classifier, and amalgamating plates. Production was very small.

Commodities (Major) - Ag, Au, Cu
Development Status: Yes; small
Deposit Model: Polymetallic veins (Cox and Singer, 1986, model 22c)

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


7 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrrhotite2.CC.10Fe1-xS
β“˜Pyrite2.EB.05aFeS2
β“˜Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3

Other Databases

Link to USGS - Alaska:HE203

Other Regions, Features and Areas containing this locality


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