Overlooking the Similkameen River

This view is taken from the Mine's main office. The mine is located atop a hill overlooking the former mill, offices and the Similkameen River bordering the Crowsnest Highway, and equidistant between Keremeos and Osoyoos.

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Entrance to the 1700 foot Adit

This adit entrance is the lowermost adit and main haulage tunnel. An exposed surface vein system was also discovered at this level.

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Overlooking the Similkameen River

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Short Adits, or “Gopher Holes”

These holes can be found throughout the property. Dating back to the 1890’s, early miners followed these highgrade Silver veins until they cut off

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Reviewing the Plan View of the Mine

The mine has five adit levels at elevations of 2600, 2500, 2400, 2200 and 1700 feet and three sublevels within the 12 plus kilometres of tunnels, subdrifts and raises.

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Latest News Releases

Silver Fields' Keremeos Update
Tuesday, May 14, 2013

Silver Fields Resources Inc. announces the Company has updated the James Laird Silver Project exploration plans for 2013 which include continued mechanized trenching and sampling on the...

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Silver Fields Extends Private Placement
Monday, April 22, 2013

Silver Fields Resources Inc. is pleased to announce the Company has requested and received TSX Venture Exchange approval to extend the closing of the private placement announced in....

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Silver Fields Closes First Tranche of Private Placement
Friday, March 01, 2013

Silver Fields Resources Inc. is pleased to announce that the Company has now closed the first tranche of the private placement announced on February 21, 2013. A total of 2,500,000 non flow through units were issued at...

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Silver Fields Resources Inc. (TSXV: SF) is an exploration company focusing on exploring for precious metals properties. The Company’s current projects are located in British Columbia. These properties consist of a number of early staged silver properties, located in the Interior of the province. All properties have been selected on the basis of promising stratigraphy and structure, documented alteration, and proximity to historical mineralized occurrences.