The Cariboo Hudson Mine

The Cariboo Hudson Mine is located at the headwaters of Pearce Creek, a feeder of the legendary Cunningham Creek.  

Gold quartz ore bodies were known on Yanks Peak and Round Top Mountain as early as the 1860s, but were not heavily exploited until the 1920s when local prospector Fred Wells explored the surface veins at Pearce Creek and began sinking shafts and adits into the newly discovered ore bodies. 

A road from Keithly Creek was upgraded, and extended down into the nearby valleys to allow heavy equipment access to the site from Barkerville.  

The Cariboo Hudson was built between 1929 and 1931 and mining properly began in 1936 after multiple issues plagued the project. By 1937 the underground workings of the Hudson had discovered the ore body had been cut away by faulting and after multiple attempts to retrace it, the mine and its equipment were shutdown, dismantled and moved to the newly built Cariboo Gold Quartz mine on Jack of Clubs Lake. The sites building laid dormant until 1950 when several camp buildings and a machine shop were moved down the valley to the Shaput Tungsten mine, but were only used sporadically.  

Gold ore at the Hudson is composed of a fine grained, chalcopyrite and phyhorite, often associated with amorphous galena and schelite stringers. Barite argentite veins are also known to be present nearby, likely an extension of the deposits located down steam at Penny Creek.