• Site banners
  • Site banners

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
S12-05Eagle Bay Unit EBQPS-79-151P Schirizzagarnet biotite muscovite schist
S12-04Eagle Bay Unit EBQPS-79-145P Schirizzamuscovite quartzite
S12-03Eagle Bay Unit EBQPS-79-153P Schirizzastaurolite muscovite quartz schist
S12-02Eagle Bay Unit EBQPS-79-146P SchirizzaChlorite sericite schist
S12-01Eagle Bay Unit EBQPS-79-152P SchirizzaStaurolite(?) chlorite muscovite schist
S11-15Shulaps Ultramafic complexDunite - wehrliteweakly layered; olive green on broken surface is probably olivine, partially serpentinized; bands of chromite
S11-14Shulaps Ultramafic complexPyroxenite(?)medium green; medium grained, all crystals are uniformly 2-3 mm, and appear to be pyroxene; non-magnetic
S11-13Shulaps Ultramafic complexDunite with clinopyroxeneolive green on broken surfaces but no crystals evident; very strongly magnetic
S11-12Shulaps Ultramafic complexWehrlitecoarse, 1 cm size euhedral olivine(?) surrounded by black clinopyroxene(?); moderately magnetic
S11-11Shulaps Ultramafic complexClinopyroxenite with orthopyroxene (by collector)coarse grained, 1 cm crystals; possibly orthopyroxene is bronze weathering, interstitial mineral seen on partly weathered surface, if that is correct, then 80% clinopyroxene; 20% orthopyroxene
S11-10Shulaps Ultramafic complexDiabase dike (swarm)fine grained; 50% feldspar; 50% pyroxene; requires hand lens to see salt-and-pepper texture; non-magnetic; similar to S11-08
S11-09Shulaps Ultramafic complex(Isotropic) Gabbrocoarse grained, 0.5 cm crystals; 70% feldspar; 30% hornblende(?) after pyroxene; submitted as "isotropic" meaning there is no evidence of layering, however there is evidence of crystal alignment
S11-08Shulaps Ultramafic complexDiabase dyke(?)near black; fresh; massive; fine grained; 50% feldspar; 50% pyroxene; non-magnetic
S11-07Shulaps Ultramafic complexFoliated serpentiniteblack; shiny; schistose; magnetic
S11-06Shulaps Ultramafic complexGabbromassive; medium grained; 70% feldspar; 30% pyroxene; non-magnetic
S11-05Shulaps Ultramafic complexGabbrofine to medium grained; salt-and-pepper texture; 60% feldspar; 40% pyroxene; non-magnetic
S11-04Shulaps Ultramafic complexSheared Pyroxenite(?)medium green; coarse grained; non-magnetic; numerous slickensided fractures
S11-03Shulaps Ultramafic complexSerpentinized peridotite(?)dense; black; strongly magnetic; serpentine on fractures
S11-02Shulaps Ultramafic complexPeridotite(?)dun weathering typical of suite; massive; no identifiable minerals other than 1% chromite evident on weathered surface; non-magnetic
S11-01Shulaps Ultramafic complexPeridotite25% olivine(?) phenocrysts 1 cm in size; resistant stubby pyroxene crystals on weathered surface but cannot be distinguished on fresh surface; non-magnetic
S10-10Purcell - Philips FmT HoyRed sandstone - siltstoneProterozoichematite red; shallow water, tidal flats deposit
T 0160 (missing)Purcell - Creston FmSpar Lake, Troy MontanaT HoyDiagenetic red-bed, mineralizedProterozoicmajor silver-copper mine
S10-09Purcell - Gateway FmT HoyLimestoneProterozoicmm scale bedding; cryptal-algal mats formed in shallow water
T0101 (missing)Purcell - Gateway FmT HoyOrthoquartziteProterozoicmassive, fluvial deposit
T 0100 (missing)Purcell - Nicol CreekT HoyAmygdaloidal basaltProterozoicvertical pipe vesicles
T 0099 (missing)Purcell - Van Creek FmT HoySiltstoneProterozoicripple marks; shallow water deposit
T 0098 (missing)Purcell - Van Creek FmT HoyMudchip brecciaProterozoicaccumulation of mu- cracked siltstone
S10-08Purcell - Kitchener FmT HoyArgillaceous limestoneProterozoicinterbedded, on 0.5 cm scale, limestone and limey argillite; molar tooth structures in carbonate, an enigmatic sedimentary structure consisting of variously shaped cracks and voids filled with a characterically uniform, equant calcite microspar; globally distributed but only in rocks of Neoarchean to Neoproterozoic age
S10-07Purcell - Base of Creston FmMoyie Lake areaT HoySiltstoneProterozoicgrey; shallow water siltstone; synerses cracks (shrinkage cracks caused by explusion of water from a gel-like substance
S10-06Purcell - Creston FmT HoyMud-cracked siltstoneProterozoicred; cm scale bedding; mud cracks visible on one bedding plane
T 0094 (missing)Purcell - Creston FmT HoyMud-cracked siltstoneProterozoic
S10-05Purcell - Creston FmT HoyGreen siltstoneProterozoicpale green; mm to cm scale beds, silty to argillaceous; reduced, shallow water deposit
S10-04Purcell - Creston FmT HoyRed siltstoneProterozoicmm to cm scale silt and mud beds; graded bedding and scour marks; shallow water deposit
S10-03Purcell - Upper Aldridge FmT HoyArgilliteProterozoicmedium dark grey; fine bedded (mm scale); deep water deposition; <1% pyrite but results in rusty weathering
S10-02Purcell - Middle Aldridge FmT HoyMiddle Aldridge marker horizonProterozoicunique bedding sequence that can be traced 100's of km
T 0089 (missing)Purcell - Middle Aldridge FmSt Eugene mine areaT HoyTurbiditeProterozoicmassive; thick bedded wacke; typical of A sequence in Bouma cycle
T 0088 (missing)Purcell - Middle Aldridge FmT HoyMoyie SillProterozoic
T 0087 (missing)Purcell - Middle Aldridge FmT HoyTurbiditeProterozoiccross-bedded (c - interval of turbidite)
S10-01Purcell - Lower Aldridge FmT HoyTurbidite siltstoneProterozoicrusty weathering turbidite and laminated siltstone; beds 3-6 cm thick
T 0085 (missing)Purcell - Lower Aldridge FmNorth Star mine areaT HoyTurbidite wackeProterozoicrusty weathering, deep water (distal) siltstone-turbidite
S9-16Bridge River ComplexMetabasalt ?dense; fine grained; chloritic; weakly magnetic
S9-15Bridge River ComplexBlack argillitetectonized
S9-14Bridge River ComplexRibbon chertfine ribbon chert with argillaceous partings; strongly tectonized, minor folds and fractured; remobilized silica veinlets
S9-13Bridge River ComplexBlack slateschistose; finely interbedded chert
S9-12Bridge River ComplexAltered basalt (greenstone)foliated; aphanitic; no calcite
S9-11Bridge River ComplexLeuco-gabbromedium grained; 60% plagioclase 2-3 mm size; non-magnetic; finer grained equivalent of above and more felsic
S9-10Bridge River ComplexGabbro40% plagioclase 0.5-1 cm size; finer grained unidentified mafic matrix; weakly magnetic
S9-09Bridge River ComplexAltered basaltdark green; fine grained; 10% secondary calcite
S9-08Bridge River ComplexAndesite?medium grey; fine grained; homogenous; no phenocrysts
S9-07Bridge River ComplexSedimentary brecciarounded to very angular fine-grained felsic clasts in grey-black argillaceous matrix

Samples in your order cart

You haven't selected any samples
Order your samples and book a viewing time.

Want to help SEG keep the Rock Room going? Donate using the button below.