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Kagati Lake Prospect, Bethel Mining District, Dillingham Census Area, Alaska, USAi
Regional Level Types
Kagati Lake ProspectProspect
Bethel Mining DistrictMining District
Dillingham Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
59° 55' 12'' North , 159° 54' 36'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
198285
Long-form identifier:
mindat:1:2:198285:8
GUID (UUID V4):
0


Location: The Kagati Lake prospect is in uplands in the headwaters of Atmugiak Creek, 5.5 miles northeast of Kagati Lake. It is at an elevation of about 3,400 feet above the small, east-headwater lake to Atmugiak Creek. It is locality 1 of Hoare and Cobb (1977) and of Cobb and Condon (1972).
Geology: The Kagati Lake prospect is within a Cretaceous granitic pluton (Hoare and Coonrad, 1978). It was discovered and prospected by 1927 (Malone, 1962) but explored mostly in the 1950s (Sainsbury and MacKevett, 1965). North-northwest-trending fractures and shear zones up to 1,200 feet long and approximately parallel to steep joints in the host granitic rock control mineralization. Cinnabar, some closely associated with realgar, stibnite, and minor orpiment, forms veinlets and fills fractures in the shear zones. Individual cinnabar masses are 2 to 24 inches wide, but are observed only for lengths up to 10 feet due to limited exposure. Quartz, some vuggy, and clay accompany the cinnabar; secondary antimony minerals and iron-oxides are also present. Frost (1990, p. C5) describes the veins as zoned with margins of blue-green to brown tourmaline needles extending into a core of quartz and calcite; cinnabar and stibnite crystals with some realgar and orpiment are scattered through quartz in the cores of the veins. Gold values up to 2.9 ppm were obtained on vein material (Frost, 1990; Gray and others, 1990).
Workings: Exploration includes pits, trenches, and dozer stripping; surface mapping was completed in the 1950s (Sainsbury and MaKevett, 1965).
Age: Late Cretaceous or Tertiary. The mineralization postdates the host granitic pluton, which yielded a K/Ar age of 71.1 +/- 2.1 Ma on biotite (Hoare and Coonrad, 1978).
Alteration: Silicification and oxidation.

Commodities (Major) - Au, Hg, Sb
Development Status: None
Deposit Model: Epithermal mercury- and antimony-bearing veins in granitic rock

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


6 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Cinnabar2.CD.15aHgS
Stibnite2.DB.05Sb2S3
Realgar2.FA.15aAs4S4
Orpiment2.FA.30As2S3
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Unclassified
'Tourmaline'-AD3G6(T6O18)(BO3)3X3Z

List of minerals for each chemical element

BBoron
B TourmalineAD3G6(T6O18)(BO3)3X3Z
CCarbon
C CalciteCaCO3
OOxygen
O CalciteCaCO3
O QuartzSiO2
O TourmalineAD3G6(T6O18)(BO3)3X3Z
SiSilicon
Si QuartzSiO2
SSulfur
S CinnabarHgS
S OrpimentAs2S3
S RealgarAs4S4
S StibniteSb2S3
CaCalcium
Ca CalciteCaCO3
AsArsenic
As OrpimentAs2S3
As RealgarAs4S4
SbAntimony
Sb StibniteSb2S3
HgMercury
Hg CinnabarHgS

Other Databases

Link to USGS - Alaska:GO011

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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