Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Flat Creek Mine (tributary of Timber Creek), Ruby Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types
Flat Creek Mine (tributary of Timber Creek)Mine
Ruby Mining DistrictMining District
Yukon-Koyukuk Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 3' 29'' North , 155° 34' 26'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
197492
Long-form identifier:
mindat:1:2:197492:1
GUID (UUID V4):
0


This mineral occurrence is not to be confused with another occurrence on a different Flat Creek (RB016), tributary to Long Creek (RB020).
Location: Flat Creek is a tributary of Timber Creek. Coordinates given are for the approximate center of tailings (1/2 mile long) marked on the Ruby A-6 quadrangle, in section 31, T. 16 S., R. 17 E., Kateel River Meridan (USGS topographic map, 1952, minor revisions in 1973). This site corresponds to location 34 of Cobb (1972 [MF405]) and location 19 of Eberlein and others (1977). The location is accurate.
Geology: The bedrock underlying Flat Creek, a tributary of Timber Creek, is phyllite (Mertie, 1936). Drilling along Flat Creek indicates a shear zone across Bonanza Creek and the lower end of Flat Creek (Pete Haggland, oral communication, 2000). The gold is found on or in the upper 6 inches of bedrock or on a false clay bedrock a short distance above the true bedrock (Mertie and Harrington, 1916). The ground consists of 40 to 50 feet of muck underlain by 2 to 30 feet of gravel. The gravel is composed of chert, vein quartz, and phyllite (Mertie and Harrington, 1916). Gold is found in narrow, irregular patches and streaks over a width of as much as 1,000 feet. The gold is rough, and most is attached to quartz. It is rarely present in nuggets heavier than half an ounce and is commonly accompanied by pyrite, rounded grains of cassiterite, magnetite, a little arsenopyrite, and barite. The barite is present near the mouth (Eberlein and others, 1977). Three assays of the gold averaged 786 parts gold per thousand and 207 parts silver per thousand (Mertie, 1936). Mining occurred at least between 1913 and 1936. In 1913 and 1914 two mines operated on Flat Creek (Eberlein and others, 1977). In the fall of 1940, John Miscovitch and others moved a D-8 Cat and dozer into Flat Creek and started building a ditch from Timber Creek and stripping a large area for hydraulicking the overburden (John Miscovitch, written communication, 2000). Flat Creek was mined by hydraulically, removing about 45 feet of overburden and using a mechanical sluice box system (Pete Haggland, oral communication, 2000). Mining continued until 1942 and also occurred from 1946 to 1954. More recent activity took place along Flat Creek between 1990 and 1993 (Swainbank and others, 1991; Bundtzen and others, 1992; Swainbank and others, 1993; Bundtzen and others, 1994).
Workings: Flat Creek was intermittently mined from 1913 until at least 1936. In the fall of 1940, John Miscovitch and others moved a D-8 Cat and dozer into Flat Creek and started building a ditch from Timber Creek and stripping a large area for hydraulicking the overburden (John Miscovitch, written communication, 2000). Mining continued until 1942 and from 1946 to 1954. Mining along Flat Creek also occurred between 1990 and 1993 (Swainbank and others, 1991; Bundtzen and others, 1992; Swainbank and others, 1993; Bundtzen and others, 1994).
Age: Quaternary.

Commodities (Major) - Au; (Minor) - Ag, Sn
Development Status: Yes
Deposit Model: Placer Au (Cox and Singer, 1986; model 39a).

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
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Cassiterite4.DB.05SnO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4

List of minerals for each chemical element

OOxygen
O BaryteBaSO4
O CassiteriteSnO2
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ArsenopyriteFeAsS
S BaryteBaSO4
FeIron
Fe ArsenopyriteFeAsS
AsArsenic
As ArsenopyriteFeAsS
SnTin
Sn CassiteriteSnO2
BaBarium
Ba BaryteBaSO4
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:RB051

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.

References

Brooks, A.H., 1915, Mineral resources of Alaska; report on progress of investigations in 1914: U.S. Geological Survey Bulletin 622, 380 p. Bundtzen, T.K., Swainbank, R.C., Clough, A.H., Henning, M.W., and Hansen, E.W., 1994, Alaska's mineral industry, 1993: Alaska Division of Geological and Geophysical Surveys Special Report 48, 84 p. Bundtzen, T.K., Swainbank, R.C., Wood, J.E., Clough, A.H., 1991 (1992), Alaska's Mineral Industry 1991: Alaska Division of Geological & Geophysical Surveys, Special Report 46, 89 p. Chapman, R.M., Coats, R.R., and Payne, T.G., 1963, Placer tin deposits in central Alaska: U.S. Geological Survey Open-File Report 239, 53 p. Cobb, E.H., 1972, Metallic mineral resources map of the Ruby quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-405, 1 sheet, scale 1:250,000. Cobb, E.H., and Chapman, R.M., 1981, Mineral occurrences (other than mineral fuels and construction materials) in the Kantishna River and Ruby quadrangles, Alaska: U.S. Geological Survey Open-File Report 81-170, 94 p. Eberlein, G.D., Chapman, R.M., Foster, H.L., and Gassaway, J.S., 1977, Map and table describing known metalliferous and selected nonmetalliferous mineral deposits in central Alaska: U.S. Geological Survey Open-File Report 77-168-D, 132 p., 1 sheet, scale 1:1,000,000. Mertie, J.B., Jr., 1936, Mineral deposits of the Ruby-Kuskokwim region, Alaska: U.S. Geological Survey Bulletin 864-C, p. 115-245. Mertie, J.B., Jr., and Harrington, G.L., 1916, Mineral resources of the Ruby-Kuskokwim region, in Brooks, A.H., and others, Mineral Resources of Alaska, Report on Progress of Investigations in 1915: U.S. Geological Survey Bulletin 642-H, p. 223-266. Swainbank, R.C., Bundtzen, T.K., and Wood, J.E., 1991, Alaska's mineral industry, 1990: Alaska Division of Geological and Geophysical Surveys Special Report 45, 78 p. Swainbank, R.C., Bundtzen, T.K., Clough, A.H., Hansen, E.W., and Nelson, M.G., 1993, Alaska's mineral industry, 19
 
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