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ROCK ROOM

Smithers Exploration Group's Collection of Cordilleran Rock Suites

Welcome to Smithers Exploration Group’s Rock Room, home to our classic collection of Cordilleran rock suites. This extensive collection of rock samples is representative of deposits and rock types from across British Columbia, with a focus on the northwest. It’s an important resource for the development of expertise on the geology of northern BC and the discovery of the next mines.

The collection was begun in the 1970s by local geologists and prospectors, as well as the BC Ministry of Mines, and was updated under the direction of former regional geologist Paul Wojdak. It is designed to give hands-on examples of the rocks that make up the regional geological framework of northern British Columbia.  We are working hard to complete our collection: if there is a particular suite you are keen to see but we do not yet have, please let us know and we will prioritize the aquisition of those samples.  If you have a suite that you would consider donating to help us fill in the gaps, please contact us.

The Rock Room occupies a spacious classroom at the Smithers Exploration Group office at #101 3423 Fulton Avenue in Smithers. We have almost 2000 rock samples catalogued, clearly labelled and stored in trays that can be removed for handling and close examination. The room is heated, well-lit and spacious .It is equipped with regular and zoom stereomicroscopes for detailed investigation.

The rock suites cover:

Call 250-877-7883 or email rockroom@smithersexplorationgroup.com if you have questions about the Rock Room or the donation requirements for samples.

SEG’s Rock Room with its Cordilleran Rock Suites will make Smithers home to a unique tool for explorationists.  It will attract industry and government attention to Smithers as a community committed to the growth of the minerals industry in BC.

Browse the Rock Room Collection

Library No.Suite NameLocationCollectorRock NameAgeDescriptionCart
D20-07Kemess SouthM RebagliatiPlagioclase micro-porphyry monzodiorite15% plagioclase, 2-3 mm, with pale green sausserite alteration; <5% hornblende, 1-2 mm; rare quartz, 1 mm microphenos; 75% pink, fine grained matrix that is probably K-feldspar; 5% quartz veins with envelope of K-feldspar and secondary biotite
D20-06Kemess SouthM RebagliatiMonzodiorite with quartz stockworkplagioclase phyric; strongly altered; 60% quartz veins; pyrite veins cut quartz veins
D20-05Kemess SouthM RebagliatiMonzodiorite, supergene alterednative copper present
D20-04Kemess SouthM RebagliatiPropylitic lapilli tuffheterolithic; clasts to 2 cm; plagioclase and amphibole crystal fragments in matrix; abundant epidote, pervasive and as veins; pervasive calcite
D20-03Kemess SouthM RebagliatiChert, tuffaceousmottled pale pink to white
D20-02Kemess SouthM RebagliatiBasaltdark green to black; very fine grained; black colour may be partly due to secondary biotite; chalcopyrite irregularly distributed, as scattered clots rather than disseminated; sparse moly associated with cpy; a few pyrite veinlets <1 mm wide
D20- 01Kemess SouthM RebagliatiPlagioclase micro-porphyry monzodiorite, strongly altered and veinedTriassic?light colour; 20% light green (sausseritized) plagioclase 1-2 mm; 10% primary quartz; 15% secondary biotite as replacement of primary mafic minerals, as envelopes to quartz veins and in quartz veins; 55% white aphanitic groundmass; vein stockwork of quartz-pyrite-chalcopyrite-molybdenite(?); veins are tectonically disrupted and broken quartz fragments are difficult to distinguish from primary quartz
D19-09Kemess NorthM RebagliatiAltered bladed plagioclase porphyry diorite(?)more altered than D19-08; black zones contain several % disseminated pyrite, plus biotite and magnetite
D19-08Kemess NorthM RebagliatiAltered bladed plagioclase porphyry diorite(?)similar to D19-06 but matrix is mottled grey to black; black areas are strongly magnetic and likely contain secondary biotite
D19-07Kemess NorthM RebagliatiPorphyritic syenite dike75% pink feldspar 1-2 mm (crowded porphyry); matrix is greenish, due to chlorite?; no quartz; reported to be post mineralization intrusion
D19-06Kemess NorthM RebagliatiBladed plagioclase porphyry diorite(?)30% plagioclase phenocrysts to 1 cm long; 70% dark, very fine grained matrix
D19-04Kemess NorthM RebagliatiChloritized andesite fragmentalmedium to dark green; very strong pervasive chlorite; quartz-anhydrite veins (identified as fluorite)
D19-04Kemess NorthM RebagliatiHydrothermal brecciaintroduced quartz dominates; much lesser pyrite, chalcopyrite, magnetite
D19-03Kemess NorthM RebagliatiHydrothermal brecciaearly quartz-pyrite (ore stage) veins are cut by gypsum and lesser anhydrite
D19-02Kemess NorthM RebagliatiPlagioclase microporphyry monzodioriteheterogenous alteration; pervasive K-feldspar alteration obliterates intrusive texture; strong pervasive secondary biotite; 3 cm anhydrite-pyrite-chalcopyrite vein; pale purple anhydrite commonly mistaken for fluorite
D19-01Kemess NorthM RebagliatiAltered andesite fragmentalTriassic?black to dark grey; 7% disseminated pyrite; anastamosing quartz veinlet with trace secondary biotite; black rock colour may be pervasive secondary biotite
D18-12Copper Mountain - SimilkameenT Richards?Hornfels volcanic brecciadark grey to black; heterolithic clasts to 3 cm, some plagioclase-phyric, one or two light grey; clast-matrix texture homogenized by contact metamorphism
D18-11Copper Mountain - SimilkameenT Richards?Stockwork veined hornfelsmottled black, white and orange; hard; relict dark biotite hornfels; intense stockwork of K-feldspar, silica and albite
D18-10Copper Mountain - SimilkameenT Richards?Altered hornfels argillite(?)light grey; hard; siliceous; relict breccia texture strongly overprinted by pervasive alteration and indistinct to clear veins of fine grained silica; minor K-spar alteration; some preserved biotite (or chlorite after biotite) remaining of hornfels. Interpreted to be argillite hornfels strongly overprinted by hydrothermal alteration
D18-09Copper Mountain - SimilkameenT Richards?K-feldspar altered hornfels?small specimen of dark hornfels (or mafic volcanic) with K-feldspar alteration
D18-08Copper Mountain - SimilkameenT Richards?K-feldspar-epidote altered mafic volcanic?similar to D18-06; host rock obscured by strong alteration; K-spar - epidote-albite veins comprise most of sample; white feldspar (2-4 mm) within K-spar areas resemble relict primary plagioclase but are most likely albite alteration; minor biotite and quartz within K-spar; no bornite or other sulphides
D18-07Copper Mountain - SimilkameenHydrothermal K-feldspar veinAndesite wallrock to 6 cm wide vein of pink K-feldspar, biotite, quartz, epidote and interstitial calcite
D18-06Copper Mountain - SimilkameenT Richards?K-feldspar-epidote altered mafic volcanic?green and pink; pervasive epidote alteration cross-cut by K-feldspar veins with chlorite envelope; minor euhedral biotite within K-feldspar; specularite(?) crystals widely disseminated within K-feldspar
D18-05Copper Mountain - SimilkameenT Richards?Fractured sericite-altered rhyolite?light grey; very fine grained; similar to D18-4 but less siliceous due to sericite and possible chlorite; strong cross-cutting fractures; minor py; one speck cpy; 1-2 cm calcite vein
D18-04Copper Mountain - SimilkameenT Richards?Rhyolite?light grey; very fine grained; siliceous; hint of breccia texture; narrow (1-2 mm) silica veinlets
D18-03Copper Mountain - SimilkameenT Richards?Biotite hornfelsed siltstonedark purply-brown; bedded; very fine grained; chlorite as patches and irregular, discontinuous veinlets with bleached envelopes
D18-02Copper Mountain - SimilkameenT Richards?Basaltdark green-black; very fine grained; non-magnetic; 10% coarse (5 mm) pyrite, fracture-controlled accompanied by minor quartz; black colour may be due to secondary biotite
D18-01Copper Mountain - SimilkameenT Richards?Mafic volcanicdark green; massive; fragmental texture is weakly visible, possibly due to hornfels overprint
D17-08Silver StandardGalena veinlate Cretaceousfine grained, bleached siltstone with disseminated pyrite and arsenopyrite(?); coarse galena fills vein opening
D17-07Silver StandardMassive sulphide ore breccialate Cretaceoussiltstone breccia healed by (in sequential order) carbonate that rims fragments, sphalerite and chalcopyrite, and finally galena and arsenopyrite
D17-06Silver StandardSiltstone hornfelslaminated; indurated; partly baked because fractures predominate over bedding
D17-05Silver StandardFelsite dikelate Cretaceousbleached quartz-biotite porphyry; fine sericite alteration; disseminated pyrite
D17-04Silver StandardCarbonaceous sandstoneJurassicblack; medium grained; unaltered
D17-03Silver StandardQuartz-siderite cemented breccialate Cretaceousfragments all uniformly bleaced siltstone
D17-02Silver StandardBleached siltstonelate Cretaceouslight grey; fine grained; massive
D17-01Silver StandardSiderite cemented breccialate Cretaceousangular breccia fragments uniformly bleached; no reaction between ore fluid and wallrock
D16-09Carlin Gold depositsManhattan pitSiltstone (or volcanic) with quartz stockworkore grade
D16-08Carlin Gold depositsBald Mountain pitSiltstone with quartz veinspink, hematitic siltstone, finely laminated; cut by vuggy quartz veins
D16-07Carlin Gold depositsGold QuarryJasperoid brecciaopen space between breccia clasts
D16-06Carlin Gold depositsCarlin MineBleached limey siltstonefinely laminated; assays to 1 oz/t Au
D16-05Carlin Gold depositsCarlin MineBleached limey siltstonefinely laminated; assays 1-2 oz/t Au
D16-04Carlin Gold depositsCarlin MineJasperoid with fine baritegrey, vuggy silica; barite reported but cannot be identified in sample, too fine grained; assays to 0.2 oz/t Au
D16-03Carlin Gold depositsCarlin MineBrecciated jasperoid veinangular clasts in dark grey silicic matrix; limonite gossan from surface weathering
D16-02Carlin Gold depositsGold QuarryChert and limey siltstonepurple-black chert in tectonic contact with light grey limey siltstone; assaysto 0.1 oz/t Au
D16-01Carlin Gold depositsCarlin MineJasperoid vein in shear zonegrey; fine grained siltstone; hard, siliceous; strongly fractured, crackled; gossan weather surface; assays up to 1 oz/t Au
D14-16Bell Copper30% coarse grained tarnished pyrite vein with trace qtz + calcite. 60% bleached biotite feldspar porphyry? Strong argillic alteration.
D14-15Bell CopperBiotite feldspar porphyry, altered and stockwork veinedEocenepervasive hydrothermal biotite in host rock which is poorly visible; stockwork of quartz-pyrite-chalcopyrite veins with K-feldspar envelope and retrograde chlorite-carbonate alteration; calcite on most fracture surfaces
D14-14Bell CopperQuartz stockworkEocene90% quartz-pyrite veins; 10% fragments with faintly visible intrusive texture but completely altered to powdery kaolinite
D14-13Bell CopperWeathered massive chalcopyriteEocene
D14-12Bell CopperChalcopyrite veinEocenepoor specimen; unrecognizeable wallrock; late coarse calcite

Samples in your order cart

Library No.Suite NameLocationCollectorRock NameAgeDescriptionCart
A5 04Argillic AlterationT RichardsArgillic spheroidal rhyolitestrong pervasive argillic alteration likely due to steam in a geothermal field; 10% spherules are mostly leached out to voids, some remaining silica and clay; iron oxidized to hematite; strong gossan weathering
D14-13Bell CopperWeathered massive chalcopyriteEocene
D14-14Bell CopperQuartz stockworkEocene90% quartz-pyrite veins; 10% fragments with faintly visible intrusive texture but completely altered to powdery kaolinite
A5 02Argillic AlterationT RichardsBladed feldspar porphyry andesite30% plagioclase laths, 1-2 cm long, pale green in colour due to sausserite (zoisite / epidote) alteration; microcrystalline groundmass is dark green, likely chlorite altered
D4-07Afton Mines - Ajax suiteAjax WestMine staffHybrid diorite (microdiorite)Up Triassicfine to medium grained, grey-green; equal proportion of chloritized mafics and plagioclase; minor py and epidote
D2-05Premier Mine2-level portalD AlldrickSemi-massive sulphideJurassic50% py, 20% sph, 1% cpy; quartz and calcite gangue
D14-16Bell Copper30% coarse grained tarnished pyrite vein with trace qtz + calcite. 60% bleached biotite feldspar porphyry? Strong argillic alteration.
A4 11Copper-Bearing PropylitesT RichardsActinolite - quartz skarn brecciadense, medium grained, prismatic actinolite with 10% rounded quartz "pebbles" that are linked by quartz-chalcopyrite stringers
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