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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
S18-38Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoicblack with brown streaks along flow direction; 5-10% plagioclase; rare (one) pyroxene crystal
S18-37Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoicblack; aphanitic; massive; trace feldspar; trace calcite amygdules
S18-36Edziza VolcanoRaspberry FmJ SoutherCalcite amygduleCenozoicradiating crystal; 4-5 cm size
S18-35Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoicas above, very sparse plagioclase crystals; flow layered
S18-34Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoicdark grey; mainly aphyric, perhaps single phenocryst per surface of specimen
S18-33Edziza VolcanoRaspberry FmJ SoutherPlagioclase phyric basaltCenozoicbrown; 25% feldspar 1.5 cm long by 0.5 cm wide, unusual honey brown colour, twinning evident on minority of crystals; sparse (<1%) tiny pyroxene or oxide crystals
S18-32Edziza VolcanoIce Peak FmJ SoutherBasaltCenozoicblack-green; grey weathering; aphanitic; 1% vesicles
S18-31Edziza VolcanoIce Peak FmJ SoutherBasaltCenozoicdark green-black; dense; massive; no vesicles; sparse phenocrysts of feldspar, pyroxene(?) that are somewhat rounded, resorbed?
S18-30Edziza VolcanoIce Peak FmJ SoutherBasaltCenozoicblack, weathers dark grey; dense; aphanitic; no vesicles
S18-29Edziza VolcanoBig Raven FmJ SoutherOlivine basaltCenozoicgrey; 5% plagioclase; 3% olivine, prominent 1 cm phenocryst; 10% vesicles
S18-28Edziza VolcanoBig Raven FmJ SoutherVesicular olivine basaltCenozoicred-brown; 10% plagioclase to 4 mm; 2% olivine, irredescent pale green
S18-27Edziza VolcanoBig Raven FmJ SoutherVesicular basaltCenozoicred-brown; 5% plagioclase laths to 1 cm; 20% vesicles; possibly minor altered pyroxene
S18-26Edziza VolcanoBig Raven FmJ SoutherVesicular olivine basaltCenozoic25% vesicles; 1% olivine; 1% feldspar crystals
S18-25Edziza VolcanoBig Raven FmJ SoutherPahoehoe (ropy) lavaCenozoicreddish-brown; strongly flow-textured; low density due to air pockets
S18-24Edziza VolcanoBig Raven FmJ SoutherOlivine basaltCenozoicblack; 10-15% olivine, 1-2 mm; 2% plagioclase, 1-2 mm size
S18-23Edziza VolcanoBig Raven FmJ SoutherOlivine basaltCenozoicblack; 2% olivine, mm size; 10% plagioclase, 1-3 mm size; 2% pyroxene(?), hard to discern; 4% vesicles
S18-22Edziza VolcanoBig Raven FmJ SoutherBasaltCenozoicdark grey; 10% plagiocase; 1% vesicles
S18-21Edziza VolcanoPillow Ridge FmJ SoutherVesicular basaltCenozoicblack; 5% plagioclase laths; 25% vesicles
S18-20Edziza VolcanoPillow Ridge FmJ SoutherVesicular basaltCenozoicvery irregular texture; xenoliths of plagioclase-pyroxene with crystals to 2 cm size; 0-25% plagioclase laths; 15-20% vesicles; matrix is glassy near vesicles
S18-19Edziza VolcanoNido FmJ SoutherOlivine basaltCenozoic20-25% olivine phenocrysts, pale to honey brown, vitreous; <5% plagioclase; 65% brown aphanitic matrix; 10% vesicles
S18-18Edziza VolcanoNido FmJ SoutherBasaltCenozoicred-brown; 2-3% plagioclase, 1-4 mm; 1% vesicles and calcite amygdules, mainly <2 mm
S18-17Edziza VolcanoNido FmJ SoutherBasalt brecciaCenozoic50% brown matrix; 50% aphyric clasts - tan, grey, black, red, vesicular, non-vesicular; clasts are angular to sub-round
S18-16Edziza VolcanoNido FmJ SoutherBasaltCenozoicgreenish-black; similar to above but aphyric
S18-15Edziza VolcanoNido FmJ SoutherOlivine basaltCenozoicgreenish-black; similar to above but more phenocrysts, 3-4% olivine and plagioclase
S18-14Edziza VolcanoNido FmJ SoutherBasaltCenozoicblack; chocolate brown weathering; mainly aphanitic, one or two feldspars
S18-13Edziza VolcanoNido FmJ SoutherTrachyteCenozoicpurple; 15% feldspar and olivine phenocrysts, 0.5 to 2 cm size; weakly flow-aligned; feldspars are twinned, olivine is amber
S18-12Edziza VolcanoNido FmJ SoutherAmygdaloidal basaltCenozoicbrown; 5% amygdules, 2 cm size, two types of fillings, radiating calcite and lesser chalcedony
S18-11Edziza VolcanoEdziza FmJ SoutherTrachyteCenozoicvery dark grey; flow foliation (layered); 1% feldspar both parallel and perpendicular to flow foliation; trachyte is reported to be predominant lithology
S18-10Edziza VolcanoEdziza FmJ SoutherTrachyteCenozoicdark grey; 1-2% plagiocase; possible pyroxene; massive texture, no vesicles
S18-09Edziza VolcanoEdziza FmJ SoutherTrachyteCenozoicmedium grey; aphyric except for one rounded feldspar megacryst 1 cm in size, apparent resorption halo; 5% irregular cavities (vesicles); trachyte is reported to be predominant lithology
S18-08Edziza VolcanoEdziza FmJ SoutherTrachyteCenozoicgrey-green; nearly aphyric, 1-2% pyroxene phenocrysts, less than mm size; trachyte is reported to be predominant lithology
S18-07Edziza VolcanoEdziza FmJ SoutherTrachyteCenozoicgreen; 5% feldspar phenocrysts, to 5 mm size; trachyte is reported to be predominant lithology
S18-06Edziza VolcanoSpectrum FmJ SoutherRhyodacite crystal tuffCenozoicgreenish-grey; <5% phenocrysts of twinned feldspar (mainly), lesser rounded quartz and minor biotite; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite)
S18-05Edziza VolcanoSpectrum FmJ SoutherRhyoliteCenozoicgrey; vesicular; flow banded; secondary quartz crystals formed in some vugs; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite)
S18-04Edziza VolcanoSpectrum FmJ SoutherAndesite - basalt lapilli tuffCenozoic80% aphanitic purple matrix; 20% tan brown aphanitic clasts, to 0.5 cm; reported to be alkali olivine basalt
S18-03Edziza VolcanoSpectrum FmJ SoutherRhyodacite ash tuffCenozoiclight grey; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite)
S18-02Edziza VolcanoSpectrum FmJ SoutherFelsic ash flow (ignimbrite)Cenozoicmedium grey; finely banded; contorted banding; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite)
S18-01Edziza VolcanoSpectrum FmJ SoutherRhyolite ashCenozoicoff-white; possible phenocrysts too small to be identified; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite)
S17-11Tagish - LabargeTeepee prospectM MihalnyukSkarn, sulphide bearingwhite to very pale green; too fine grained to identify minerals; reported to contain grossularite, tremolite, diopside, epidote; 5-10% irregularly distributed cobaltite, arsenopyrite, magnetite (minor, non-magnetic); patchy cobalt bloom (eurythrite)
S17-10Tagish - LabargeCrine prospectM MihalnyukQuartz-pyrite-arsenopyrite veingold bearing
S17-09Tagish - Labarge104M/8,9M MihalnyukBiotite granite (lKg)Cretaceouswhite-grey; medium-coarse grained; 40% quartz; 55% feldspar, appears to be all plagioclase; 5% biotite
S17-08Tagish - Labarge104M/8,9M MihalnyukRhyolite (MVr)white-grey; massive; aphanitic
S17-07Tagish - Labarge104M/8,9M MihalnyukBiotite-muscovite-plagioclase-quartz schist (PPMb)dark grey; knots of quartz vaguely resemble garnet porphyroblasts; crinkle folds shown by biotite; derived from greywacke
S17-06Tagish - Labarge104M/8,9M MihalnyukChlorite-actinolite schist (PPMa)green; finely laminated on mm scale; derived from mafic volcanic flow or tuff
S17-05Tagish - Labarge104M/8,9M MihalnyukMarble (PPMm)pale to medium grey; tight folding of resistant bands
S17-04Tagish - Labarge104M/8,9M MihalnyukHornblendite (JKh)Jura-Cretaceousblack; >95% very coarse hornblende; 5 cm aligned crystals; 1-2% interstitial feldspar, sausseritized (epidote altered), pale green
S17-03Inklin / Labarge GrpStikine River areaM Mihalnyuk & T RichardsVolcanic sandstone / greywackeLower to Mid-Jurassicgrey; abundant fine muddy matrix (i.e. greywacke); fine pebbles of white (acidic) and greenish (basic) volcanics; feldspar and mafic clasts; immature greywacke
S17-02Inklin / Labarge GrpM Mihalnyuk & T RichardsGreywacke / sandstoneLower to Mid-Jurassicgrey; common rip-up clasts of shale, aligned parallel to bedding; platey fracture corresponds to slatey cleavage, at high angle to bedding
S17-01Inklin/ Labarge GrpM Mihalnyuk & T RichardsFeldspathic volcanic sandstonelower to Mid-Jurassicgrey; little matrix; minor shale fragments; slatey cleavage prominently developed
S16-11Phyllitegreen to tan with metamorphic pyrite (originally diagenetic?) cubes to <= 1cm associated with calcite +- quartz

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