Dixie; Galena-Gold Prospect, Willow Creek Mining District, Matanuska-Susitna Borough, Alaska, USAi
Regional Level Types | |
---|---|
Dixie; Galena-Gold Prospect | Prospect |
Willow Creek Mining District | Mining District |
Matanuska-Susitna Borough | Borough |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
61° 49' 11'' North , 149° 17' 23'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Fishhook | 4,679 (2011) | 8.9km |
Buffalo Soapstone | 855 (2011) | 15.2km |
Farm Loop | 1,028 (2011) | 21.5km |
Tanaina | 8,197 (2011) | 22.6km |
Lakes | 8,364 (2011) | 23.6km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Mat-Su Rock and Mineral Club | Palmer, Alaska | 26km |
Mindat Locality ID:
197228
Long-form identifier:
mindat:1:2:197228:6
GUID (UUID V4):
ea1d8977-5dc8-4738-97dd-58ed5c2fe775
Location: 2,500 ft southeast of head of Purches Creek, within the Purches Creek drainage. Accurate within 1,000 ft. Locality 8 of Chapin (1914, plate IV), locality 16 of Cobb (1972), and locality 13 of MacKevett and Holloway (1977).
Geology: At least one foot of 'good ore' contains chalcopyrite, pyrite, galena, and free gold on surface (Capps, 1919). An 8.5 ft wide pegmatitic vein strikes N 55 W, and dips 55 SE. The coarse, border material consists of quartz, orthoclase, muscovite, and particles of chalcopyrite along the borders. Central part of vein is milky quartz cut by irregular stringers of chalcopyrite and a little bornite (Chapin, 1921). Country rock is the Late Cretaceous Willow Creek Pluton, a zoned pluton: the outer part consists of hornblende quartz diorite and lesser hornblende tonalite; the core consists of hornblende-biotite granodiorite, and lesser hornblende-biotite quartz monzodiorite and biotite quartz monzonite. Wall-rock alteration within a few inches of the vein is intense, but seldom extends more than 10 to 12 inches beyond the quartz filling. Sericitization and carbonate alteration predominate, but there is some pyritization and in the outer parts of the alteration zone chloritization is present (Ray, 1954).
Workings: Three claims first staked in 1917 on surface expression of 1 ft of 'good ore'. Very little development reported, the prospect was explored in one place by an open-cut across vein Chapin (1921).
Age: Late Cretaceous or younger; the mineralized host is the Late Cretaceous Willow Creek Pluton.
Alteration: Wall-rock alteration within a few inches of the vein is intense, but seldom extends more than 10 to 12 inches beyond the quartz filling. Sericitization and carbonate alteration predominate, but there is some pyritization and in the outer parts of the alteration zone chloritization is present (Ray, 1954).
Commodities (Major) - Au, Cu, Pb
Development Status: None
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
8 valid minerals.
Detailed Mineral List:
β Bornite Formula: Cu5FeS4 |
β Chalcopyrite Formula: CuFeS2 |
β Galena Formula: PbS |
β Gold Formula: Au |
β Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
β Orthoclase Formula: K(AlSi3O8) |
β Pyrite Formula: FeS2 |
β Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
β | Gold | 1.AA.05 | Au |
Group 2 - Sulphides and Sulfosalts | |||
β | Bornite | 2.BA.15 | Cu5FeS4 |
β | Chalcopyrite | 2.CB.10a | CuFeS2 |
β | Galena | 2.CD.10 | PbS |
β | Pyrite | 2.EB.05a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
β | Quartz | 4.DA.05 | SiO2 |
Group 9 - Silicates | |||
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | Orthoclase | 9.FA.30 | K(AlSi3O8) |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | Oxygen | |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Orthoclase | K(AlSi3O8) |
O | β Quartz | SiO2 |
Al | Aluminium | |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Orthoclase | K(AlSi3O8) |
Si | Silicon | |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Orthoclase | K(AlSi3O8) |
Si | β Quartz | SiO2 |
S | Sulfur | |
S | β Bornite | Cu5FeS4 |
S | β Chalcopyrite | CuFeS2 |
S | β Galena | PbS |
S | β Pyrite | FeS2 |
K | Potassium | |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
K | β Orthoclase | K(AlSi3O8) |
Fe | Iron | |
Fe | β Bornite | Cu5FeS4 |
Fe | β Chalcopyrite | CuFeS2 |
Fe | β Pyrite | FeS2 |
Cu | Copper | |
Cu | β Bornite | Cu5FeS4 |
Cu | β Chalcopyrite | CuFeS2 |
Au | Gold | |
Au | β Gold | Au |
Pb | Lead | |
Pb | β Galena | PbS |
Other Databases
Link to USGS - Alaska: | AN023 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Wrangellia DomainDomain
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