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:
- Plutonic
- Volcanic
- Sedimentary
- Metamorphic
- Stratigraphy
- Mineral Deposits and Ore Deposit Types
- Rock-forming and Ore Minerals
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 Name | Location | Collector | Rock Name | Age | Description | Cart |
|---|---|---|---|---|---|---|---|
| S18-38 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | black with brown streaks along flow direction; 5-10% plagioclase; rare (one) pyroxene crystal | |
| S18-37 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | black; aphanitic; massive; trace feldspar; trace calcite amygdules | |
| S18-36 | Edziza Volcano | Raspberry Fm | J Souther | Calcite amygdule | Cenozoic | radiating crystal; 4-5 cm size | |
| S18-35 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | as above, very sparse plagioclase crystals; flow layered | |
| S18-34 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | dark grey; mainly aphyric, perhaps single phenocryst per surface of specimen | |
| S18-33 | Edziza Volcano | Raspberry Fm | J Souther | Plagioclase phyric basalt | Cenozoic | brown; 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 | |
| S18-32 | Edziza Volcano | Ice Peak Fm | J Souther | Basalt | Cenozoic | black-green; grey weathering; aphanitic; 1% vesicles | |
| S18-31 | Edziza Volcano | Ice Peak Fm | J Souther | Basalt | Cenozoic | dark green-black; dense; massive; no vesicles; sparse phenocrysts of feldspar, pyroxene(?) that are somewhat rounded, resorbed? | |
| S18-30 | Edziza Volcano | Ice Peak Fm | J Souther | Basalt | Cenozoic | black, weathers dark grey; dense; aphanitic; no vesicles | |
| S18-29 | Edziza Volcano | Big Raven Fm | J Souther | Olivine basalt | Cenozoic | grey; 5% plagioclase; 3% olivine, prominent 1 cm phenocryst; 10% vesicles | |
| S18-28 | Edziza Volcano | Big Raven Fm | J Souther | Vesicular olivine basalt | Cenozoic | red-brown; 10% plagioclase to 4 mm; 2% olivine, irredescent pale green | |
| S18-27 | Edziza Volcano | Big Raven Fm | J Souther | Vesicular basalt | Cenozoic | red-brown; 5% plagioclase laths to 1 cm; 20% vesicles; possibly minor altered pyroxene | |
| S18-26 | Edziza Volcano | Big Raven Fm | J Souther | Vesicular olivine basalt | Cenozoic | 25% vesicles; 1% olivine; 1% feldspar crystals | |
| S18-25 | Edziza Volcano | Big Raven Fm | J Souther | Pahoehoe (ropy) lava | Cenozoic | reddish-brown; strongly flow-textured; low density due to air pockets | |
| S18-24 | Edziza Volcano | Big Raven Fm | J Souther | Olivine basalt | Cenozoic | black; 10-15% olivine, 1-2 mm; 2% plagioclase, 1-2 mm size | |
| S18-23 | Edziza Volcano | Big Raven Fm | J Souther | Olivine basalt | Cenozoic | black; 2% olivine, mm size; 10% plagioclase, 1-3 mm size; 2% pyroxene(?), hard to discern; 4% vesicles | |
| S18-22 | Edziza Volcano | Big Raven Fm | J Souther | Basalt | Cenozoic | dark grey; 10% plagiocase; 1% vesicles | |
| S18-21 | Edziza Volcano | Pillow Ridge Fm | J Souther | Vesicular basalt | Cenozoic | black; 5% plagioclase laths; 25% vesicles | |
| S18-20 | Edziza Volcano | Pillow Ridge Fm | J Souther | Vesicular basalt | Cenozoic | very irregular texture; xenoliths of plagioclase-pyroxene with crystals to 2 cm size; 0-25% plagioclase laths; 15-20% vesicles; matrix is glassy near vesicles | |
| S18-19 | Edziza Volcano | Nido Fm | J Souther | Olivine basalt | Cenozoic | 20-25% olivine phenocrysts, pale to honey brown, vitreous; <5% plagioclase; 65% brown aphanitic matrix; 10% vesicles | |
| S18-18 | Edziza Volcano | Nido Fm | J Souther | Basalt | Cenozoic | red-brown; 2-3% plagioclase, 1-4 mm; 1% vesicles and calcite amygdules, mainly <2 mm | |
| S18-17 | Edziza Volcano | Nido Fm | J Souther | Basalt breccia | Cenozoic | 50% brown matrix; 50% aphyric clasts - tan, grey, black, red, vesicular, non-vesicular; clasts are angular to sub-round | |
| S18-16 | Edziza Volcano | Nido Fm | J Souther | Basalt | Cenozoic | greenish-black; similar to above but aphyric | |
| S18-15 | Edziza Volcano | Nido Fm | J Souther | Olivine basalt | Cenozoic | greenish-black; similar to above but more phenocrysts, 3-4% olivine and plagioclase | |
| S18-14 | Edziza Volcano | Nido Fm | J Souther | Basalt | Cenozoic | black; chocolate brown weathering; mainly aphanitic, one or two feldspars | |
| S18-13 | Edziza Volcano | Nido Fm | J Souther | Trachyte | Cenozoic | purple; 15% feldspar and olivine phenocrysts, 0.5 to 2 cm size; weakly flow-aligned; feldspars are twinned, olivine is amber | |
| S18-12 | Edziza Volcano | Nido Fm | J Souther | Amygdaloidal basalt | Cenozoic | brown; 5% amygdules, 2 cm size, two types of fillings, radiating calcite and lesser chalcedony | |
| S18-11 | Edziza Volcano | Edziza Fm | J Souther | Trachyte | Cenozoic | very dark grey; flow foliation (layered); 1% feldspar both parallel and perpendicular to flow foliation; trachyte is reported to be predominant lithology | |
| S18-10 | Edziza Volcano | Edziza Fm | J Souther | Trachyte | Cenozoic | dark grey; 1-2% plagiocase; possible pyroxene; massive texture, no vesicles | |
| S18-09 | Edziza Volcano | Edziza Fm | J Souther | Trachyte | Cenozoic | medium 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 | |
| S18-08 | Edziza Volcano | Edziza Fm | J Souther | Trachyte | Cenozoic | grey-green; nearly aphyric, 1-2% pyroxene phenocrysts, less than mm size; trachyte is reported to be predominant lithology | |
| S18-07 | Edziza Volcano | Edziza Fm | J Souther | Trachyte | Cenozoic | green; 5% feldspar phenocrysts, to 5 mm size; trachyte is reported to be predominant lithology | |
| S18-06 | Edziza Volcano | Spectrum Fm | J Souther | Rhyodacite crystal tuff | Cenozoic | greenish-grey; <5% phenocrysts of twinned feldspar (mainly), lesser rounded quartz and minor biotite; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite) | |
| S18-05 | Edziza Volcano | Spectrum Fm | J Souther | Rhyolite | Cenozoic | grey; vesicular; flow banded; secondary quartz crystals formed in some vugs; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite) | |
| S18-04 | Edziza Volcano | Spectrum Fm | J Souther | Andesite - basalt lapilli tuff | Cenozoic | 80% aphanitic purple matrix; 20% tan brown aphanitic clasts, to 0.5 cm; reported to be alkali olivine basalt | |
| S18-03 | Edziza Volcano | Spectrum Fm | J Souther | Rhyodacite ash tuff | Cenozoic | light grey; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite) | |
| S18-02 | Edziza Volcano | Spectrum Fm | J Souther | Felsic ash flow (ignimbrite) | Cenozoic | medium grey; finely banded; contorted banding; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite) | |
| S18-01 | Edziza Volcano | Spectrum Fm | J Souther | Rhyolite ash | Cenozoic | off-white; possible phenocrysts too small to be identified; reported to be microporphyritic comendite to pantellerite (peralkaline, sodic rhyolite) | |
| S17-11 | Tagish - Labarge | Teepee prospect | M Mihalnyuk | Skarn, sulphide bearing | white 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) | ||
| S17-10 | Tagish - Labarge | Crine prospect | M Mihalnyuk | Quartz-pyrite-arsenopyrite vein | gold bearing | ||
| S17-09 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Biotite granite (lKg) | Cretaceous | white-grey; medium-coarse grained; 40% quartz; 55% feldspar, appears to be all plagioclase; 5% biotite | |
| S17-08 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Rhyolite (MVr) | white-grey; massive; aphanitic | ||
| S17-07 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Biotite-muscovite-plagioclase-quartz schist (PPMb) | dark grey; knots of quartz vaguely resemble garnet porphyroblasts; crinkle folds shown by biotite; derived from greywacke | ||
| S17-06 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Chlorite-actinolite schist (PPMa) | green; finely laminated on mm scale; derived from mafic volcanic flow or tuff | ||
| S17-05 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Marble (PPMm) | pale to medium grey; tight folding of resistant bands | ||
| S17-04 | Tagish - Labarge | 104M/8,9 | M Mihalnyuk | Hornblendite (JKh) | Jura-Cretaceous | black; >95% very coarse hornblende; 5 cm aligned crystals; 1-2% interstitial feldspar, sausseritized (epidote altered), pale green | |
| S17-03 | Inklin / Labarge Grp | Stikine River area | M Mihalnyuk & T Richards | Volcanic sandstone / greywacke | Lower to Mid-Jurassic | grey; abundant fine muddy matrix (i.e. greywacke); fine pebbles of white (acidic) and greenish (basic) volcanics; feldspar and mafic clasts; immature greywacke | |
| S17-02 | Inklin / Labarge Grp | M Mihalnyuk & T Richards | Greywacke / sandstone | Lower to Mid-Jurassic | grey; common rip-up clasts of shale, aligned parallel to bedding; platey fracture corresponds to slatey cleavage, at high angle to bedding | ||
| S17-01 | Inklin/ Labarge Grp | M Mihalnyuk & T Richards | Feldspathic volcanic sandstone | lower to Mid-Jurassic | grey; little matrix; minor shale fragments; slatey cleavage prominently developed | ||
| S16-11 | Phyllite | green to tan with metamorphic pyrite (originally diagenetic?) cubes to <= 1cm associated with calcite +- quartz |
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