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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
T6-06Epithermal Gold-Silver veinsLawyers, ToodoggoneD LefebureBrecciated feldspar porphyry with quartz veinsJurassicmultiple episodes of quartz veins; veins are banded to coxcomb texture
T6-05Epithermal Gold-Silver veinsLawyers, ToodoggoneD LefebureBanded quartz vein in tuffJurassicsymmetrically banded, 1.5 cm chalcedonic quartz vein in pinkish-brown tuff; core of vein has some crystalline quartz with hint of amythest colour
T6-04Epithermal Gold-Silver veinsLawyers, ToodoggoneD LefeburePlagioclase phyric tuffJurassiclayered; pink feldspar in reddish grounmass; feldspar in crystal-rich beds; feldspar is likely hematitized plagioclase, crystals do not resemble primary K-feldspar
T6-03Epithermal Gold-Silver veinsLawyers, ToodoggoneD LefebureDacite tuffJurassiclight brown; 10% plagioclase crystals, 1 mm size, orange in colour due to cloudy hematite; groundmass has pervasive chlorite (propylitic alteration)
T6-02Epithermal Gold-Silver veinsAl prospect, ToodoggoneD LefebureQuartzJurassicwhite; drusy, minor open space; vein or silicified rock?
T6-01Epithermal Gold-Silver veinsAl prospect, ToodoggoneD LefebureClay-alunite alterationJurassicwhite; massive; fine grained; light density; bladed crystals evident on one weathered surface
T5-12SkarnEpidote-calcite skarnparent rock is andesite with abundant secondary calcite
T5-11SkarnFrench Mine, HedleyBiotite hornfels argillitedark purplish-brown; very fine grained; colour indicates pervasive metamorphic biotite
T5-10SkarnFrench Mine, HedleyK-feldspar-epidote-chalcopyrite skarn40% K-feldspar; 40% epidote; 15% chalcopyrite
T5-09SkarnNickel Plate mine, HedleyQuartz-eye rhyolite dikevery pale grey; massive; aphanitic; 3-4% quartz phenocrysts; trace arsenopyrite
T5-08SkarnNickel Plate mine, HedleySulphide skarn75% pyrrhotite; 10% chalcopyrite; 10% pyrite; 5% arsenopyrite
T5-07SkarnHedleyCopperfield conglomerate marker horizoncobbles to 8 cm; biotite hornfels of argillaceous matrix; composition is wrong to develop skarn
T5-06SkarnFrench Mine, HedleyDioritedark grey-green; fine-medium grained; 25% hornblende; 75% indistinguishable feldspathic groundmass
T5-05SkarnBlue Grouse, Vancouver Is.Feldspar porphyry dioritegreen; medium grained; 60% feldspar; 25% hornblende; intrusion responsible for skarn development
T5-04SkarnBlue Grouse, Vancouver Is.Garnet-epidote-actinolite skarn40% epidote; 25% garnet; 25% actinolite; 10% quartz
T5-03SkarnBob deposit, Banks IslandArsenopyrite skarn50% quartz; 30% arsenopyrite; 10% sphalerite; 5% chalcopyrite
T5-02SkarnFrench Mine, HedleyGarnet skarn85% pink-brown garnet; 5% pyroxene; 5% quartz; 5-10% calcite
T5-01SkarnTasuMagnetite skarnTriassic95% magnetite; 5% pyrite plus chalcopyrite
T4-11SkarnBlue Grouse, Vancouver Is.Garnet-epidote skarnone rock cut in two, one half with no label; brown weathered makes minerals garnet and epidote difficult to recognize; 15% interstitial calcite
T4-10SkarnFrench mine, HedleyMagnetite skarn95% magnetite; 5% pyrite plus chalcopyrite
T4-09SkarnNickel Plate, HedleySulphide skarncoarse grained; massive; 40% arsenopyrite; 30% pyrite; 20% pyrrhotite; 10% chalcopyrite
T4-08SkarnFrench mine, HedleyPyroxene-bornite skarndense; fine grained; 10% bornite; 1% chalcopyrite
T4-07SkarnBlue Grouse, Vancouver Is.Dioritesame rock as in C2
T4-06SkarnFrench mine, HedleyGarnet-calcite skarn25% garnet
C1 05 (missing)SkarnFrench mine, Hedley
T4-04SkarnBob deposit, Banks IslandHornblende granodiorite85% feldspar (predominantly plagioclase, no K-feldspar observed); 10% hornblende; <1% biotite
T4-03SkarnBob deposit, Banks IslandSulphide skarn70% arsenopyrite; 10% sphalerite; 5% pyrite; 15% quartz; reported to contain 0.59 oz/t Au, 0.29 oz/t Ag, 9.98% Zn
T4-02SkarnBob deposit, Banks IslandGarnet skarn90% garnet; 2% pyroxene; 6% calcite
T4-01SkarnTasuMagnetite skarnTriassic95% magnetite; 5% pyrite plus chalcopyrite; same as C2 01
T3-11Manto & SedexMudstone with barite laminaeDevonianwhite barite as fine laminations, <1 mm thick in black mudstone
T3-10Manto & SedexSullivanBedded pyrite-pyrrhotite in shaleProterozoicsame as B1 07
T3-09Manto & SedexCirqueMassive bariteDevoniancrudely bedded; bedding disrupted; recrystallized barite; minor galena
T3-08Manto & SedexMt. AlcockSemi-massive bariteDevonianvery fine grained; dense; 5% fine galena (similar to B1 05)
T3-07Manto & SedexMidwayMassive sulphideDevonian70% pyrite; 20% galena; 5% sphalerite; not bedded
B2 01 (missing)Manto & SedexMidwayBedded shaleDevonian
T3-06Manto & SedexSullivanBedded pyrite-pyrrhotite in shaleProterozoicblack, very fine grained shale or cherty shale(?); finely bedded sulphide beds, some predominantly pyrite, some pyrrhotite and others mixed; evidence of sulphide recrystallization leading to increased grain size
T3-05Manto & SedexCirqueMassive sulphideDevonianmassive pyrite with 6% sphalerite, 1% galena
T3-04Manto & SedexMt. AlcockMassive bariteDevonianpale grey; disrupted bedding and coarse recrystallization of barite; 3-5% galena seams
T3-03Manto & SedexMt. AlcockMassive sulphideDevoniandark grey; very fine grained; dense; reported to comprise pyrite, sphalerite and galena but only galena can be identified; probably contains barite
B1 03 (missing)Manto & SedexMidwayShale breccia with pyrite-carbonate cement
T3-02Manto & SedexMidwayTectonic shale breccia with sulphide cementDevonianidentical specimens; brittle breccia healed by coarse pyrite, galena and sphalerite
T3-01Manto & SedexMidwayShale with pyrite bedDevoniandrill core of very thin bedded shale3 cm thick pyrite bed; pyrite is recrystallized into minute cubes
A2 12 (missing)VMSTyee deposit, Mt Sicker, Vancouver Is.FerrocreteRecent
T2-11VMSLynx deposit, Myra FallsKuroko black ore (bedded pyrite-chalcopyrite-sphalerite)Devonian30% sphalerite; 30% pyrite; 10% chalcopyrite; 20% silica gangue
T2-10VMSLenora Pit, Mt SickerChert with pyrite-chalcopyrite veinschert is well fractured and broken with in-filling of sulphide veins to 2 cm wide; pyrite to chalcopyrite ration is 10:1
T2-09VMSHW deposit, Myra FallsMassive pyritic oreDevonianlayered but only vaguely bedded; 60% pyrite; 5% chalcopyrite;30% silica (and perhaps barite); no galena seen but likely a few % sphalerite
T2-08VMSWindy CraggyChlorite-pyrrhotite tuff10% pyrrhotite, finely bedded within massive chlorite, likely a fine tuff or basalt-derived mud; weakly magnetic
T2-07VMSKutchoRecrystallized massive pyriteLower Triassic80% fine to coarse pyrite; the coarse pyrite (to 1 cm) is associated with remobilized chalcopyrite (3%), bornite (3%) and coarse quartz (10%)
T2-06VMSLenora Pit, Mt SickerChalcopyrite oreDevonian25% chalcopyrite in silica-barite groundmass; quartz and carbonate "clasts" these are tectonic in origin, detached from enclosing beds during deformation and recrystallization of sulphides and is called durchbewegung texture
T2-05VMSTyee deposit, Mt Sicker, Vancouver Is.Kuroko black oreDevonian60% sphalerite (and galena?); 20% pyrite; 15% barite; <5% calcite as durchbewegung clasts

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