The Painter Mine is a gold mine located in Idaho county, Idaho.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Mine Info
Satelite View
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Painter Mine MRDS details
Site Name
Primary: Painter Mine
Secondary: Surprise Group
Secondary: Idaho Newsome
Commodity
Primary: Gold
Secondary: Silver
Tertiary: Lead
Location
State: Idaho
County: Idaho
District: Salmon River District
Land Status
Land ownership: National Primitive Area
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Administrative Organization: Idaho Primitive Area
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Robert V. Hansberger
Home Office: Idaho
Years: 1973 -
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Underground
Discovery Year: 1935
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Northern Rocky Mountains
Physiographic Detail: Salmon River Mountains
Mineral Deposit Model
Not available
Orebody
Form: LENSES AND STRINGERS
Structure
Type: L
Description: Intense Fracture System
Alterations
Alteration Type: L
Alteration Text: Silicification, Fe Oxides
Rocks
Name: Quartz Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Late Cretaceous
Name: Quartz Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous
Analytical Data
Analytical Data: CHIP, DUMP AND GRAB SAMPLES CONTAINED UP TO 3.95 OZ AU/TON AND UP TO 1.52 OZ AG/TON
Materials
Ore: Galena
Gangue: Quartz
Gangue: Pyrite
Comments
Comment (Reserve-Resource): Limited Potential Estimated
Comment (Location): Near Confluence Of Little Five Mile Creek And Salmon River, In Bottom Of Salmon R. Canyon
Comment (Development): 4 Patented Claims; Mill; Shaft, Head Frame, Hoist House, Aerial Tramway On East Side Of River, Shop And Oil Storage Shed On The West Side
Comment (Workings): 5 Adits, 2 Trenches, 1 Pit On East Side; 1 Adit, 2 Trenches, 1 Pit On West Side
Comment (Geology): Andesite Dikes Trend Generally East And Dip South
Comment (Commodity): Two Selected Samples Were Collected. One Contained 40.43 Grams Gold And 21.58 Grams Silver Per Tonne. The Second Sample Assayed 135 Gram Gold Per Tonne.
References
Reference (Deposit): WFOC Mineral Property File 016 049 0243
Reference (Deposit): 1970 Recon P. L. Weis And Others, Bulletin 1353-C
Reference (Deposit): Lorain, S. H., 1938, Gold Mining And Milling In Idaho County: USBM Inf. Circ. 7039, 90 P.
Reference (Deposit): 1938 Recon USBM Inf. Circ. 7039
Reference (Deposit): Weis, P. L., Schmitt, L. J., And Tuchek, E. T., 1972, Mineral Resources Of The Salmon River Breaks Primitive Area, Idaho: USGS Bulletin 1353 - C, P. 23 - 27
Reference (Deposit): Cater, F. W., And Others, 1973, Mineral Resources Of The Idaho Primitive Area And Vicinity, Idaho: USGS Bulletin 1304, 431 P.
Reference (Production): Cater, F. W., And Others, 1973, Bulletin 1304.
Reference (Deposit): 1973 Recon F. W. Cater And Others, Bulletin 1304
Idaho Gold
"Where to Find Gold in Idaho" looks at the density of modern placer mining claims along with historical gold mining locations and mining district descriptions to determine areas of high gold discovery potential in Idaho. Read more: Where to Find Gold in Idaho.