![]() Places to see in Alaska before you die include: What places in Alaska should I see before I die? Nestled in the woods outside of Talkeetna, the outlandish architecture of a private residence has garnered the nickname the “Dr. This amusement park was once a junkyard now scattered with old arcade games, a Santa Claus rocket, and the largest mukluk in the world. In Tok, check out the whimsical Mukluk Land deemed the "Most Alaskan place in Alaska" by locals. Built with 1,000 tons of ice and snow this museum features ice sculptures and a bar where guests sip cocktails while admiring the works of art. An hour north of Fairbanks is the stunning Chena Hot Springs resort home to the dazzling Aurora Ice Museum. When sightseeing in Alaska, allow time to check out some of the unique manmade attractions as well. ![]() You could spend a lifetime trekking our state’s majestic natural landscapes and still not see everything. The best man-made attractions in Alaska include: What are the best man-made attractions in Alaska? The settlement was once home to 200 residents but has been a ghost town since the 1970s, making it an unforgettably eerie ghost town. About 40 miles off the west coast of Alaska is King Island where travelers can find the remnants of an abandoned Inupiat village. Tucked away on the Homer Spit is a little-known abandoned boat graveyard easily accessible along the 4.5-mile walk down to Kachemak Bay. The astounding glacier views and striking stoney beaches of the Kenai Peninsula make it a popular tourist destination in Alaska and the charming town of Homer is a perfect basecamp to explore the region. Visiting abandoned places can make you feel as if you’ve discovered a forgotten time capsule and adventurous explorers will find many deserted destinations all across The Last Frontier. Geological Survey Open-File Report 76-633, 72 p.Can I visit any abandoned places in Alaska?Ībandoned places to visit in Alaska include: Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Circle quadrangle, Alaska: U.S. Geological Survey Professional Paper 625-D, 25 p., 1 plate. Reference (Deposit): Chapman, R.M., and Foster, R.L., 1969, Lode mines and prospects in the Fairbanks district, Alaska: U.S. Geological Survey Open-File Report 51-46, 43 p. Reference (Deposit): Killeen, P.L., and Mertie, J.B., 1951, Antimony ore in the Fairbanks District, Alaska: U.S. Geological Survey Open-File Report 76-819, 241 p. Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Livengood quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-413, 2 sheets, scale 1:250,000. ![]() Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Livengood quadrangle, Alaska: U.S. Reference (Deposit): Prindle, L.M., 1910, Auriferous quartz veins in the Fairbanks district: U.S. Reference (Deposit): Brooks, A.H., 1916, Antimony deposits of Alaska: U.S. Reference (Deposit): Freeman, C.J., 1992, 1991 Golden Summit project final report, volume 2: Historical summary of lode mines and prospects in the Golden Summit project area, Alaska: Avalon Development Corp., 159 p. The Mother Lode prospect was examined as a possible source of antimony in 1942 but no additional exploration was conducted due to insufficient tonnage potential (Killeen and Mertie, 1951). ![]() The prospect was idle in 1916 and was noted to be associated with a horizontal structure which may have been parallel to foliation (Brooks, 1916 B 649). 33 B 649).? the stibnite contains less that $1 per ton in gold (0.05 ounces of gold per ton) but the grade of the granite porphyry is unknown. There are also some vitreous quartz grains buried in the stibnite some of these grains showed crystal terminations (Brooks, 1916, p. The aggregates are highly weathered, and a little pyrite occurs with the stibnite. Specimens of ore from this deposit are made up of a granular aggregate of stibnite (Brooks, 1916, p. The stibnite occurs as pods and veinlets in the schist and as a surface coating on the dike contact (Prindle, 1910). Alteration Text: Stibnite aggregates are highly oxidized and sericite alteration was observed in the granite porphyry dike.Ĭomment (Reference): Primary Reference = Brooks, 1916 (B 649)Ĭomment (Deposit): Model Name = Stibnite vein (Cox and Singer model 27d).Ĭomment (Geology): Geologic Description = The prospect consists of a sericitized granite porphyry dike which cuts a stibnite-bearing schist.
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