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Gulch Creek and East Fork Sixmile Creek Mine, Hope Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Gulch Creek and East Fork Sixmile Creek MineMine
Hope Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 46' 34'' North , 149° 24' 0'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Hope192 (2017)20.4km
Girdwood2,250 (2017)22.4km
Moose Pass219 (2014)32.1km
Cooper Landing289 (2017)39.4km
Primrose111 (2006)44.4km
Mindat Locality ID:
197847
Long-form identifier:
mindat:1:2:197847:9
GUID (UUID V4):
0


Location: This site represents a gold placer mine at and near the confluence of Gulch and lower East Fork Sixmile Creeks. The creeks are located in T. 8 N., R. 1 W., of the Seward Meridian. The map site is just northeast of the Seward Highway, about 1.25 miles southeast of the Hope road turnoff. This is location 142 of Cobb and Richter (1972), location 166 of MacKevett and Holloway (1977), location 14-15 of Cobb and Tysdal (1980), and location P-73 of Jansons and others (1984). This location is accurate to within 300 feet.
Geology: Gulch Creek and lower East Fork Sixmile Creek occupy narrow bedrock canyons along most of their length and contain thin, discontinuous gravel deposits. The bedrock in these drainages is slate and sandstone of the Valdez Group of Late Cretaceous age(Nelson and others, 1985). Gravels in a low bench, mined at the mouth of Gulch Creek, are composed of pebbles and boulders of slate, sandstone, and granite and have a clay matrix (Tysdal, 1978 [MF-880B]). Mining about 1.5 miles upstream worked old channel gravels consisting of horizontally stratified gravel having a locally compact clay and sand matrix (Tysdal, 1978 MF-880-B]). Gravels in the active steam bed range from loose and sandy on the surface, to clay cemented, with bouldery gravel near bedrock. Some of the boulders are 5 feet or more feet in diameter. Fine gold is disseminated throughout the gravels, but the pay streak is on bedrock and in fractures and is accompanied by sticky, tan clay (Jansons and others, 1984). The gold is flat, smooth, and medium coarse to coarse (Johnson, 1912). Nuggets as heavy as 5 ounces have been recovered from Gulch Creek (Jansons and others, 1984).
Workings: Prior to 1906, the placer was worked mainly by pick and shovel. Hydraulic mining predominated from 1906 through 1917. Most of the gold was taken from the mouth of Gulch Creek and from East Fork SixmileCreek just below its confluence with Gulch Creek. East Fork Sixmile Creek has been worked mainly between Gulch Creek and Sixmile Creek (Moffit, 1906). In 1911, two hydraulic plants were in operation. The lower, smaller plant operated at the junction of Gulch and East Fork all season using an 8-inch pipe with a 2.5-inch nozzle. A 4,000-foot-long, 2-foot-wide ditch provided water. The gravel was piped into two lead boxes and then into a string of nine,12-foot-long, 1-foot-wide sluice boxes set with pole riffles (Johnson, 1912). The upper plant, situated a short distance above the mouth of Gulch Creek, was not in operation when Johnson visited in 1912. There, the gold-saving apparatus consisted of a string of 11 sluice boxes with a 3-foot- square cross section laid on bedrock (Martin and others, 1915). In 1917, two men were hydraulic mining at the mouth of Gulch Creek (Johnson, 1919 [B 692-C, p. 175-176]). In the early 1980's, the U.S. Bureau of Mines collected suction dredge samples at the head of Gulch Creek. They yielded 0.0006 to 0.0034 ounce of gold per hour. Two other samples from upper Gulch Creek contained 0.0008 to 0.0296 ounce of gold per cubic yard. Nine placer samples consisting of surface alluvium collected from the canyon of lower East Fork Sixmile Creek, contained 0.0019 to 0.015 ounce of gold per cubic yard (Jansons and others, 1984). Since the early 1980's small-scale suction dredging has become a popular mining method and occurs intermittently up to the present time (C. S. Huber, oral communication, 2000).
Age: Quaternary.
Production: The total estimated production is 1,000 to 2,500 ounces of gold, of which as much as 250 ounces has been produced since 1975 (Jansons and others, 1984).
Reserves: The quantity of the gravel both on the benches and in the active stream channel is limited. No estimate of reserves is available.

Commodities (Major) - Au
Development Status: Yes; small
Deposit Model: Placer Au (alluvial) (Cox and Singer, 1986; model 39a)

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au

List of minerals for each chemical element

AuGold
Au Native GoldAu

Other Databases

Link to USGS - Alaska:SR029

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., 1909, The mining industry in 1908: U.S. Geological Survey Bulletin 379-A, p. 21-62. Brooks, A.H., 1915, Mineral resources of Alaska; report on progress of investigations in 1914: U.S. Geological Survey Bulletin 622, 380 p. Brooks, A.H., 1916, Mineral resources of Alaska, report on progress of investigations in 1915: U.S. Geological Survey Bulletin 642, 279 p. Cobb, E.H., and Richter, D.H., 1972, Metallic mineral resources map of the Seward quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-466, 2 sheets, scale 1:250,000. Cobb, E.H., and Tysdal, R.G., 1980, Summaries of data on and list of references to metallic and selected nonmetallic mineral deposits in the Blying Sound and Seward quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-621, 276 p. Hoekzema, R.P., and Sherman, G.E., 1983, Mineral investigations in the Chugach National Forest, Alaska (Peninsula study area): U.S. Bureau of Mines in-house report; held at U.S. Bureau of Land Management Alaska State Office, Anchorage, 524 p. Jansons, Uldis, Hoekzema, R.B., Kurtak, J.M., and Fechner, S.A., 1984, Mineral occurrences in the Chugach National Forest, southcentral Alaska: U.S. Bureau of Mines Mineral Land Assessment 5-84, 218 p., 2 sheets, scale 1:250,000. Johnson, B.L., 1912, Gold deposits of the Seward-Sunrise region, Kenai Peninsula: U.S. Geological Survey Bulletin 520-E, p. 131-173. Johnson, B.L., 1919, Mining on Prince William Sound: U.S. Geological Survey Bulletin 692-C. MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected non-metalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-A, 99 p., 1 sheet, scale 1:1,000,000. Martin, G.C., Johnson, B.L., and Grant, U.S., 1915, Geology and mineral resources of Kenai Peninsula, Alaska: U.S. Geological Survey Bulletin 587, 243 p. Moffit, F.H., 1906, Gold fields of the Turnagain Arm region: U.S. Geol
 
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