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 |
---|---|---|---|---|---|---|---|
T12-18 | Industrial Minerals | K-feldspar porpyry granite (decorative stone) | 20% K-feldspar phenocrysts to 5 cm; 30% coarse plagioclase (1 cm) and 1% hornblende (1 cm); 50% medium grained matrix of quartz, plagioclase, K-feldspar and mafic (hornblende?) | ||||
T12-17 | Industrial Minerals | D Lefebure | Carbonatite | grey-brown; fine grained; featureless calcite / dolomite; widely dispersed purple fluorite | |||
T12-16 | Industrial Minerals | Lempiere | D Lefebure | Sovite (medium to coarse calcite rock with variable accessory amphibole, biotite, pyrite, pyrochlore and fluorite) | light brown; massive; fine grained calcite matrix; 5% light green to grass-green acicular amphibole(?) phenocrysts; 3% clots of magnetite | ||
T12-15 | Industrial Minerals | Lempiere | D Lefebure | Intrusive dolomite (carbonatite) | Second piece of T12-15; light brown; massive; reacts to acid when powdered; 10% green-black pyroxene(?) which weathers brown; interstitial, patchy, white unknown mineral | ||
T12-15 | Industrial Minerals | Aley prospect, Northern Rockies | D Lefebure | Intrusive dolomite (carbonatite) | light brown; fine grained; reacts to acid when powdered; 5% dark green pyroxene(?); 3% white patchy (interstitial) unknown mineral | ||
T12-14 | Industrial Minerals | unknown | D Lefebure | Bentonite | soft; crumbly; in plastic bag | ||
T12-13 | Industrial Minerals | unknown | D Lefebure | Serpentine | near black on cut surface; foliated; slippery to touch | ||
T12-12 | Industrial Minerals | Nicholson mine prospects | D Lefebure | Quartzite | white and pale grey alternating beds; bedded on cm scale | ||
T12-11 | Industrial Minerals | Quesnel area | D Lefebure | Talc | light grey to white; foliated; soapy (slippery) to touch | ||
T12-10 | Industrial Minerals | a) Texada Island b) Lost Ck, Kootenays | D Lefebure | Limestone | a) grey; massive; fine grained; featureless; a few white calcite veinlets b) white; massive; medium grained; high purity | ||
T12-09 | Industrial Minerals | Crawford Bay | D Lefebure | Dolomite | white; massive; medium grained | ||
T12-08 | Industrial Minerals | Quesnel area | D Lefebure | Diatomite | chalkly, crumbly; layered; very light; accumulation of marine diatoms | ||
T12-07 | Industrial Minerals | Parson | D Lefebure | Barite vein | white; coarse grained; massive; high density | ||
T12-06 | Industrial Minerals | Empire Valley, BC | D Lefebure | Perlite | 5% light brown feldspar; pearly lustrous matrix of hydrated glass | ||
T12-05 | Industrial Minerals | a) Rock Candy b) Oliver c) Aley | D Lefebure | Fluorspar (fluorite) | a) light, bright green; very coarse; euhedral; drusy cavities b) clear, colourless, coarse, associated with quartz c) purple, medium grained in dark green ultramafic (hornblendite or pyroxenite?) | ||
T12-04 | Industrial Minerals | Texada Island | D Lefebure | Wollastonite | white to pale green rock; wollastonite is white, very coarse, acicular, somewhat radiating crystals; pale green colour may be from a calc-silicate such as diopside | ||
T12-03 | Industrial Minerals | Baymag mine, Kootenays | D Lefebure | Magnesite | white to light grey; coarse grained; massive; moderate high density | ||
T12-02 | Industrial Minerals | Lussier River, Kootenays | D Lefebure | Gypsum | light grey and darker grey laminae (beds) on mm to cm scale; one carbon stylolite | ||
T12-01a T12-01b | Industrial Minerals | Falkland BC | D Lefebure | a) Anhydrite b) Gypsum | anhydrite is laminated with alternating pale grey and white bands, 1 cm thick; gypsum is white and massive | ||
T11-19 | Porphyry deposits | Bell mine, Babine district | D Lefebure | Biotite feldspar porphyry granodiorite | 50 Ma? | Fresh rock, unaltered; 40% plagioclase phenocrysts, 1-2 mm; 3% biotite phenocrysts; rare hornblende; 60% fine groundmass assumed to contain quartz and feldspar | |
T11-18 | Porphyry deposits | Whiting Creek, Tahtsa area | D Lefebure | Andesite, stockwork veined | host rock is dark green, very fine grained; stockwork veins of K-feldspar, quartz and pyrite | ||
T11-17 | Porphyry deposits | Granisle mine | D Lefebure | Biotite hornfels argillite | dark brown; very fine grained; stockwork of fractures, some narrow core of pyrite, have bleached, biotite-destructive envelopes; contact metamorphic biotite converted to clay, in the fringe of the copper deposit | ||
T11-16 | Porphyry deposits | Poplar, Houston area | D Lefebure | Granite' | primary minerals are altered, rock name is approximate; 60% feldspar altered to sericite; 25% quartz; no mafic minerals remain; veinlet of quartz and chalcopyrite | ||
T11-15 | Porphyry deposits | Climax, Colorado | D Lefebure | Breccia | two stages of silica introduction; early silica is fine grained and cements wallrock fragments; fragments exhibit pervasive K-feldspar alteration; late silica occurs as vein of coarse grained quartz, muscovite and biotite, the biotite is altered to chlorite | ||
T11-14 | Porphyry deposits | Endako mine | D Lefebure | Granite' | 140 Ma ? | vein of magnetite and chalcopyrite with envelope of pervasive K-feldspar alteration; no molybdenite, therefore atypical of the deposit | |
T11-13 | Porphyry deposits | Glacier Gulch, Smithers | D Lefebure | Intrusive Rhyolite | 50 Ma? | fine-medium grained, quartz-rich; veinlets of quartz, molybdenite, magnetite and pyrite | |
T11-12 | Porphyry deposits | Granisle mine | D Lefebure | Granite' | 50 Ma? | coarse grained; 20% quartz; 80% feldspar, much is hydrothermal K-feldspar so that rock cannot be properly named; 1 cm veins of quartz, K-feldspar, chalcopyrite, pyrite; cpy is also disseminated, 6% total chalcopyrite | |
T11-11 | Porphyry deposits | Whiting Creek, Tahtsa area | D Lefebure | Quartz eye porphyry | white, fine grained groundmass of 60% quartz and 40% feldspar but very difficult to estimate; no mafics; fracture veinlets of quartz, molybdenite, minor pyrite | ||
T11-10 | Porphyry deposits | Bell mine, Babine district | D Lefebure | Breccia | 50 Ma? | completely clay altered fragments, cannot determine original rock; a few fragments contain narrow quartz veinlets; cement is fine quartz and pyrite | |
T11-09 | Porphyry deposits | Poplar, Houston area | D Lefebure | Biotite hornblende granodiorite | 10% quartz; 80% feldspar; 10% chloritized hornblende and biotite; no significant alteration | ||
T11-08 | Porphyry deposits | Glacier Gulch, Smithers | D Lefebure | High silica alteration zone | 50 Ma? | 95% quartz; 4% molybdenite on fractures; 1% pyrite | |
T11-07 | Porphyry deposits | Granisle mine | D Lefebure | Biotite feldspar porphyry granodiorite | Paleozoic | grey BFP, details obscured by weathering; wide-spaced network of hairline pyrite fractures with 0.5-1 cm clay alteration envelopes | |
T11-06 | Porphyry deposits | Poplar, Houston area | D Lefebure | Granitic | buff to pink; medium grained; pervasive sericite alteration; quartz-pyrite-chalcopyrite veinlet with narrow K-feldspar halo in wallrock; later cross-cutting kaolinite-clay fracture | ||
T11-05 | Porphyry deposits | Climax, Colorado | D Lefebure | High silica alteration zone | 80% quartz, all introduced?; 20% altered wallrock fragments; 2% molybdenite; trace pyrite | ||
T11-04 | Porphyry deposits | Whiting Creek, Tahtsa area | D Lefebure | Granitic, altered and mineralized | 70% feldspar; 20% quartz; 10% chlorite after mafics; patchy biotite may be relict primary or hydrothermal; quartz-chlorite veinlets; pyrite on fractures | ||
T11-03 | Porphyry deposits | Endako mine, Main zone | D Lefebure | Quartz monzonite | 140 Ma ? | coarse grained; 25% quartz; 40% plagioclase; 30% K-feldspar; 5% hornblende plus biotite; molybdenite fractures | |
T11-02 | Porphyry deposits | Granisle mine | D Lefebure | Biotite feldspar porphyry granodiorite | 50 Ma? | medium grained; 25% plagioclase feldspar, 2-3 mm; 2% biotite, 2 mm; rare hornblende; veinlets of quartz - K-feldspar - chalcopyrite | |
T11-01 | Porphyry deposits | Bell mine, Babine district | D Lefebure | Vein stockwork in unknown rock | 50 Ma? | veins of coarse pyrite and chalcopyrite cut a fine grained, pervasively sericite altered rock that does not appear to be intrusive, could be sedimentary or volcanic | |
I1 01 (missing) | Porphyry deposits | Endako mine | D Lefebure | Biotite granodiorite | 140 Ma ? | ||
T10-12 | Base metal veins | Grouse Mtn, Houston area | D Lefebure | Bladed feldspar porphyry dike | 50 Ma? | 20% plagioclase laths, 1 cm size; fine grained dark grey groundmass; distinctly similar to Goosly Lake trachyandesite lava flows south of Houston | |
T10-11 | Base metal veins | Silver Queen, Houston area | D Lefebure | Feldspar porphyry dike | 60% feldspar altered to clay; rare biotite phenocrysts; 40% fine groundmass, presumably containing quartz | ||
T10-10 | Base metal veins | Grouse Mtn, Houston area | D Lefebure | Diabase dike | medium gray; salt-and-pepper texture; fine grained mesh of 50% feldspar and 50% hornblende(?) | ||
T10-09 | Base metal veins | Cronin, Smithers area | D Lefebure | Gossan | surface weathered rock; decomposed | ||
T10-08 | Base metal veins | Duthie mine, Smithers | D Lefebure | Granite' | 25% sericite-altered feldspar;75% very fine matrix of quartz-feldspar | ||
T10-07 | Base metal veins | Cronin, Smithers area | D Lefebure | Rhyolite (two pieces) | aphanitic host rock to Cronin veins; sulphides as disseminations and weak veinlets, galena and pyrite | ||
T10-06 | Base metal veins | Cronin, Smithers area | D Lefebure | Breccia vein | clasts of volcanic rock and early stage quartz vein, in second stage quartz-sphalerite-pyrite vein | ||
T10-05 | Base metal veins | Duthie mine, Smithers | D Lefebure | Breccia vein | wallrock fragments of bleached, sericitic volcanic rock; cemented by coarse sphalerite, pyrite and quartz | ||
T10-04 | Base metal veins | New Moon, Nanika area | D Lefebure | Quartz-galena vein | no host rock; mainly galena, subordinate pyrite | ||
T10-03 | Base metal veins | Duthie mine, Smithers | D Lefebure | Sphalerite vein | very coarse grained; minor quartz and pyrite; no wallrock | ||
T10-02 | Base metal veins | Grouse Mtn, Houston area | D Lefebure | Andesite | green; fine grained; vein of chalcopyrite, sphalerite, bornite, pyrite, quartz and calcite; no wallrock alteration |
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