| Deposit ID | 10400396 |
|---|---|
| Record type | Deposit |
| Mineralized Area | Rattlesnake Hills gold area |
| Current site name | Rattlesnake Hills Gold property |
| Alternate or previous names | Lost Muffler |
| Point of reference | Ore Body |
|---|---|
| Geographic coordinates: | -107.31345, 42.73745 (WGS84) |
| Location accuracy | 1000(meters) |
| Relative position | GPS at one of several outcrops above the buried ore bodies. Approximately 48 miles west of Casper at UTM 328400 ? 4712440 (NAD27 CONUS), access is made by turning north from WY State Highway 220 onto the Rattlesnake Hills Road. A drive of approximately 16 miles reaches the turnoff into the\nproperty in Section 36, T32N, R88W. |
Political divisions (FIPS codes)
Natrona(county)
Wyoming(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Barlow Gap(quadrangle 1:24,000 scale)
Rattlesnake Hills(quadrangle 1:100,000 scale)
Casper(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Sweetwater(hydrologic unit)
North Platte(hydrologic accounting unit)
North Platte(hydrologic subregion)
Missouri(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management WY)
Bureau of Land Management WY BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Wyoming | Natrona |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 032N | 088W | 24 | E2 | Wyoming |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Model code | 84 |
|---|---|
| USGS model code | 22b |
| Deposit model name | Alkaline Au-Te (Au-Ag-Te veins) |
| Mark3 model number | 80 |
| Ore Body (1) | -107.31345, 42.73745 |
|---|
| Development status | Prospect |
|---|---|
| Significant | Yes |
| Discovery year | 1982 |
| Discoverer | W. Dan Hausel |
| Production years | Still (2010) in exploration phase, not yet in production. |
| District name | Rattlesnake Hills |
|---|
| Type | Joint Venture Owner-Op |
|---|---|
| Owner | Evolving Gold |
| Interest | 100 |
| Home office | 1980?1075 West Georgia Street\nVancouver, BC V6E 3C9 \nwww.evolvinggold.com\nT. 604.685.6375\nF. 604.909.1163\nToll free 866.604.3864\ninfo@evolvinggold.com\n\n \n \n |
| Year | 2010 |
| Type | Unknown |
|---|---|
| Owner | Crescent Resources |
| Last year | 2010 |
| Type | In-situ |
|---|---|
| Estimate year | 2010 |
| Remarks | There is not yet sufficient information to project a mineral resource at the Rattlesnake project. |
Site visit. Sept. 2009
Hausel, 1996b
www.evolvinggold.com
Ray, G.E., 2008, The geology and gold mineralization at the Rattlesnake Hills property, Natron County, Wyoming, USA (UTM Zone 13 T0310650-4732850) NAD27 CONUS, A national intruments 43-101 Technical Report for Evolving Gold Corp, 666 Burrard St, Suite 725, Vancouver, BC, CANADA V6C 2X8: available online from sedar.com, 44 p. (Technical report, ammended Feb 18, 2008)
| Subject category | Comment text |
|---|---|
| Deposit | The following two types of Au mineralization occur on the Rattlesnake claims: Type 1: Gold hosted by Fe-rich chert horizons in the Archean basement, which is currently considered to have a low economic potential, and Type 2: Disseminated, micron-size Au mineralization related to, and largely hosted by the Eocene-age Rattlesnake Hills Alkalic Complex, particularly the diatreme breccias. This type has a very high economic potential and will be the focus of exploration efforts by Evolving Gold Corp. (NI 43-101, p. 3 or p. 7 of 44) |
| General | "The dominant trend of the steeply northerly dipping metamorphic foliation and structures in the Archean basement is NW-SE to WNW-ESE. This basement trend is transected by younger NE-SW to northerly-striking, steeply-dipping faults that apparently controlled the distribution and orientation of some Eocene alkaline plugs and dikes. Thus, areas where these two sets of major structures intersect are regarded as favorable places for exploration. Also present are several sub-circular, moderately inclined fractures that appear to circle some of the alkalic plugs and diatreme breccia pipes. These may represent either ring fractures related to the intrusion of the stocks or be related to post-eruption slumping. These curvilinear features are economically important as they have controlled some of the potassic feldspar alteration and Au mineralization." (NI-43-101, p. 7 of 44). |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 06-JUN-10 | Wilson, Anna B. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.