The Modoc No 6 is a tin mine located in Lander county, Nevada.
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.
Modoc No 6 MRDS details
Site Name
Primary: Modoc No 6
Commodity
Primary: Tin
Location
State: Nevada
County: Lander
District: Izenhood
Land Status
Not available
Holdings
Not available
Workings
Type: Underground
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Deposit Type: Vein
Operation Type: Unknown
Discovery Year: 1914
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Basin And Mountains
Mineral Deposit Model
Model Name: Rhyolite-hosted Sn
Orebody
Form: TABULAR
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: The Tin-Bearing Belt Is Marked By Red-Stained Or Bleached Silicitied Rhyolite.
Rocks
Name: Rhyolite
Role: Host
Age Type: Host Rock
Age Young: Miocene
Analytical Data
Not available
Materials
Ore: Cassiterite
Gangue: Opal
Gangue: Tridymite
Gangue: Sanidine
Gangue: Quartz
Gangue: Chalcedony
Comments
Comment (Deposit): TIN WAS DISCOVERED IN 1914 DEVELOPEMENT CONSIST OF A 50 FOOT DEEP INCLINED SHAFT. THIS SHAFT FOLLOWS THE DIP OF FOUR NEARLY PARALLEL VEINLETS. SEE FRIES (1944) FOR GEOLOGIC MAP OF THE PROSPECT ; INFO.SRC : 1 PUB LIT
Comment (Development): TIN DISCOVERED IN 1914; INCLINED SHAFT SUNK 50 FEET
Comment (Deposit): 4 NEARLY PARALLEL VEINLETS; CASSITERITE-BEARING QUARTZ VEINLETS, LENSES, AND FRACTURE COATINGS
Comment (Workings): INCLINED SHAFT
Comment (Geology): THE TIN DEPOSITS CONSIST OF CASSITERITE BEARING QUARTZ VEINLETS, LENSES AND FRACTURE COATINGS IN RHYOLITE ALONG AN EAST TRENDING BELT ABOUT 2 MILES LONG AND 1/2 MILE WIDE. THE WALL ROCKS ARE UNALTERRED, AND THERE IS LITTLE BRECCIATION AS THE FRACTURES ARE DISCONTINUOUS AND UNDERWENT INSIGNIFICANT MOVEMENT. THE VEINLETS HAVE AN OPEN TEXTURE AND APPEAR AS INCRUSTATIONS OF THE WALLS OF CROSS AND PARALLEL FISSURES. THE INCRUSTATIONS ARE LARGELY SPECULARITE AND CASSITERITE
References
Reference (Deposit): STAGER H. K. (1977) GEOLOGY & MINERAL DEPOSITS OF LANDER CO., NEV., N.B.M. BULL 88
Reference (Deposit): VANDERBERG W. O. (1939) RECON OF MINING DISTRICTS IN LANDER CO. NEV, USBM 1.C 7043
Reference (Deposit): FRIES C. (1941) TIN DEPOSITS OF NORTHERN LANDER CO. NEV., USGS BULL 931-C
Nevada Gold
Nevada has a total of 368 distinct gold districts. Of the of those, just 36 are major producers with production and/or reserves of over 1,000,000 ounces, 49 have production and/or reserves of over 100,000 ounces, with the rest having less than 100,000 ounces. Read more: Gold Districts of Nevada.
