Ore controlCinnabar Is Finely Divided In Opalite Boulders Which Probably Are Residual Material In The Upper, Weathered Portions Of A Mineralized Fault Zone
Materials
Ore mineralsCinnabar
Geology
Host rockFelsic Volcanic Rock
AlterationOpalite, Clay Alteration
Economic & production
Development statusOccurrence
Discovery year1936
Identification
Deposit ID10040286
MRDS IDM054991
RegionNA
Data scoreC
Coordinates42.32374, -120.80497
References
BROOKS, H. C., 1963, QUICKSILVER IN OREGON: OREGON DEPT. OF GEOLOGY AND MINERAL INDUSTRIES, BULL. 55, 223 P