This was adopted by Canyon Assets & Newmont Gold. Since gold-bearing constructions on this region lie parallel to almost parallel to foliation; thus, any drainage that cuts foliation will sample these gold-bearing structures and the foliation will present natural riffles at bedrock. There can be evidence at the Carissa mine that the shears continue to nice depth: so there is a continuous supply for detrital gold for placers within the region. Shear zones just like the Carissa lode are necessary as these continue to feed gold into drainages in the greenstone belt. Little Atlantic Gulch, a tributary of Large Atlantic gulch, lies west and parallel to Huge Atlantic Gulch and cuts the same rock and shear zones. Drill information by EV helps a central excessive grade mineralized zone surrounded by a low grade gold halo in a large tonnage gold deposit. The info supports a central high grade mineralized zone surrounded by a low grade gold halo producing a large tonnage gold deposit that can seemingly be minable by open pit and underground mining. This mineralized structure was also intersected to depths as great as 930 ft. King) standing to the best of shear zone. On the Carissa, past drilling by Consolidated McKinney Assets recognized a highly anomalous, 80-foot-large zone at depth.
Drilling so far has identified a mineralized body that has a 1440 ft strike size that is 640 ft wide and 1760 ft deep. Current drilling by Evolving Gold intersected a big auriferous ore body in sections 24 and 25, T 32N, R88W. When the lode was mined, only the excessive-grade ore was profitable at low gold prices, and miners left an unlimited, low-grade, resource in place. One of many principal lode deposits, the Golden Leaf group included the Golden Leaf, Priscilla, Hillside Placer, Wadams, Wallace, French, and Excelsior mines. I guess my fascination with mines developed throughout my faculty years, and specifically, I used to be fascinated by igneous and metamorphic rocks in addition to diamond deposits, greenstone belts, gold, porphyry copper, and gemstones. Staatz, M.H.,1983, Geology and descriptions of thorium and uncommon earth deposits within the southern Bear Lodge Mountains, northeastern Wyoming: U.S. Placer manufacturing from the Butte district, nevertheless, has been over-shadowed by the overall output of byproduct gold recovered from the mining of lode deposits of copper, lead, and zinc. Hausel, W.D., 1986, Preliminary report on the geology and gold mineralization of the South Go granite-greenstone terrain, Wind River Mountains, western Wyoming (USA), in Workshop on the Tectonic Evolution of Greenstone Belts: Lunar and Planetary Institute, Houston, Texas, p.
Hausel, W.D., 1985, Geology and gold mineralization of the South Go granite-greenstone terrain, western Wyoming: Utah Geological Association 1985 Guidebook, p. Hausel, W.D., 1991, Economic Geology of the South Move Granite-Greenstone Belt, Wind River Mountains, Western Wyoming.Geological Survey of Wyoming Report of Investigations 44, 129 p. Hausel, W.D., 1986, Preliminary report on the geology and gold mineralization of the South Pass greenstone belt, Wind River Mountains, Wyoming: Society of Mining Engineers of AIME Preprint 86-15, 10 p. Society of SME. 374 p. A stockwork along the southwestern margin of the RSH was anomalous. Gold was found in Montana in 1852, but it surely wasn’t till ten years later that the precious steel was present in important quantities at Grasshopper Creek in extreme southwestern Montana that resulted in a mining camp named Bannack (45o09’31″N;112o59’50″W) that resulted in the primary of several gold rushes to the state. The principal placer districts lie in southwestern Montana. Parts of Rock Creek were mined from 1933 to 1941. Pre-1933 gold placer mining operations on Rock Creek had been possible localized hydraulic operations designed to scrub gold from slopes of adjacent hill sides. When i mapped South Pass, I came throughout two prospectors (Buddy Presgrove and Hank Hudspeth) exploring for gold in Smith Gulch (42°31’3″N; 108°42’19″W) with backhoe and trommel.
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