Blog entry by Wallace Chism
We drove into the guts of the Medicine Bow Nationwide Forest to learn the way and where we should search for gold and diamonds. Diamonds have been found on Cortez Creek to the northwest of Douglas Creek by a gold prospector from Saratoga Wyoming named Paul Boden in 1977. Kimberlitic indicator mineral anomalies (notably pyrope garnet) have been also found at several locations within the forest since the primary diamonds have been discovered. However we could not find water (it didn't matter that the positioning was sitting adjacent to a creek that had diamonds in it, and that the two kimberlites we needed to mine had shear zones containing water, we couldn't get water rights and the county needed us to maneuver the mill someplace close to Ft. The ditch was constructed to haul water from Lake Christina 12 miles to the west in the excessive peaks of the Wind River Mountains to the South Go area for hydraulic mining. Hausel, W.D., 2001, The South Pass gold placers, western Wyoming: International California Mining Journal, v.70, no. 8, p.
In 1861, another group of prospectors started mining along Willow Creek, 15 miles west of Strawberry Creek. Once i began mapping in the South Pass greenstone belt in the 1980s, I was fairly impressed by the scale of the belt and amazed that such an vital district had remained largely unmapped and poorly explored in trendy times. All remained unmapped and solely partially explored till the 1980s and 1990s. The creator mapped all of them with the exception of Elmer’s Rock, which was mapped by Graff and others (1982). If you loved this information and you would certainly like to get even more info relating to leading companies for gold ira accounts (oglasi-oglasi.com) kindly visit the internet site. For probably the most half, greenstone belts are formed of darkish to black rocks with some dark inexperienced rocks that are difficult to differentiate and solely a handful of geologists find nice joy in the problem of unraveling these complex geological puzzles. Wyoming remained a wilderness that few settlers dared to journey into. Day, W.C., Hill, R.H., Kulik, D.M., Scott, D.C., and Hausel, W.D., 1989, Mineral assets of the Sweetwater Canyon wilderness study area, Fremont County, Wyoming: U.S.
Hausel, W.D., Gregory, R.W., Motten, R.H., and Sutherland, W.M., 2003, Geology of the Iron Mountain Kimberlite District & Close by Kimberlitic Indicator Mineral Anomalies in Southeastern Wyoming: Wyoming State Geological Survey Report of Investigations 54, 42 p. Hausel, W.D., 1986, Preliminary report on the geology and gold mineralization of the South Move greenstone belt, Wind River Mountains, Wyoming: Society of Mining Engineers of AIME Preprint 86-15, 10 p. 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. The metamorphic grade in the South Go area is favorable for quite a lot of aluminuous gems including garnet, andalusite, sillimanite, cordierite, ruby and sapphire. Love, J.D., Antweiler, J.C., and Mosier, E.L., 1978, A new look at the origin and quantity of the Dickie Springs-Oregon Gulch placer gold on the south end of the Wind River Mountains: Wyoming Geological Association Guidebook, p.