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 |
|---|---|---|---|---|---|---|---|
| D20-07 | Kemess South | M Rebagliati | Plagioclase micro-porphyry monzodiorite | 15% plagioclase, 2-3 mm, with pale green sausserite alteration; <5% hornblende, 1-2 mm; rare quartz, 1 mm microphenos; 75% pink, fine grained matrix that is probably K-feldspar; 5% quartz veins with envelope of K-feldspar and secondary biotite | |||
| D20-06 | Kemess South | M Rebagliati | Monzodiorite with quartz stockwork | plagioclase phyric; strongly altered; 60% quartz veins; pyrite veins cut quartz veins | |||
| D20-05 | Kemess South | M Rebagliati | Monzodiorite, supergene altered | native copper present | |||
| D20-04 | Kemess South | M Rebagliati | Propylitic lapilli tuff | heterolithic; clasts to 2 cm; plagioclase and amphibole crystal fragments in matrix; abundant epidote, pervasive and as veins; pervasive calcite | |||
| D20-03 | Kemess South | M Rebagliati | Chert, tuffaceous | mottled pale pink to white | |||
| D20-02 | Kemess South | M Rebagliati | Basalt | dark green to black; very fine grained; black colour may be partly due to secondary biotite; chalcopyrite irregularly distributed, as scattered clots rather than disseminated; sparse moly associated with cpy; a few pyrite veinlets <1 mm wide | |||
| D20- 01 | Kemess South | M Rebagliati | Plagioclase micro-porphyry monzodiorite, strongly altered and veined | Triassic? | light colour; 20% light green (sausseritized) plagioclase 1-2 mm; 10% primary quartz; 15% secondary biotite as replacement of primary mafic minerals, as envelopes to quartz veins and in quartz veins; 55% white aphanitic groundmass; vein stockwork of quartz-pyrite-chalcopyrite-molybdenite(?); veins are tectonically disrupted and broken quartz fragments are difficult to distinguish from primary quartz | ||
| D19-09 | Kemess North | M Rebagliati | Altered bladed plagioclase porphyry diorite(?) | more altered than D19-08; black zones contain several % disseminated pyrite, plus biotite and magnetite | |||
| D19-08 | Kemess North | M Rebagliati | Altered bladed plagioclase porphyry diorite(?) | similar to D19-06 but matrix is mottled grey to black; black areas are strongly magnetic and likely contain secondary biotite | |||
| D19-07 | Kemess North | M Rebagliati | Porphyritic syenite dike | 75% pink feldspar 1-2 mm (crowded porphyry); matrix is greenish, due to chlorite?; no quartz; reported to be post mineralization intrusion | |||
| D19-06 | Kemess North | M Rebagliati | Bladed plagioclase porphyry diorite(?) | 30% plagioclase phenocrysts to 1 cm long; 70% dark, very fine grained matrix | |||
| D19-04 | Kemess North | M Rebagliati | Chloritized andesite fragmental | medium to dark green; very strong pervasive chlorite; quartz-anhydrite veins (identified as fluorite) | |||
| D19-04 | Kemess North | M Rebagliati | Hydrothermal breccia | introduced quartz dominates; much lesser pyrite, chalcopyrite, magnetite | |||
| D19-03 | Kemess North | M Rebagliati | Hydrothermal breccia | early quartz-pyrite (ore stage) veins are cut by gypsum and lesser anhydrite | |||
| D19-02 | Kemess North | M Rebagliati | Plagioclase microporphyry monzodiorite | heterogenous alteration; pervasive K-feldspar alteration obliterates intrusive texture; strong pervasive secondary biotite; 3 cm anhydrite-pyrite-chalcopyrite vein; pale purple anhydrite commonly mistaken for fluorite | |||
| D19-01 | Kemess North | M Rebagliati | Altered andesite fragmental | Triassic? | black to dark grey; 7% disseminated pyrite; anastamosing quartz veinlet with trace secondary biotite; black rock colour may be pervasive secondary biotite | ||
| D18-12 | Copper Mountain - Similkameen | T Richards? | Hornfels volcanic breccia | dark grey to black; heterolithic clasts to 3 cm, some plagioclase-phyric, one or two light grey; clast-matrix texture homogenized by contact metamorphism | |||
| D18-11 | Copper Mountain - Similkameen | T Richards? | Stockwork veined hornfels | mottled black, white and orange; hard; relict dark biotite hornfels; intense stockwork of K-feldspar, silica and albite | |||
| D18-10 | Copper Mountain - Similkameen | T Richards? | Altered hornfels argillite(?) | light grey; hard; siliceous; relict breccia texture strongly overprinted by pervasive alteration and indistinct to clear veins of fine grained silica; minor K-spar alteration; some preserved biotite (or chlorite after biotite) remaining of hornfels. Interpreted to be argillite hornfels strongly overprinted by hydrothermal alteration | |||
| D18-09 | Copper Mountain - Similkameen | T Richards? | K-feldspar altered hornfels? | small specimen of dark hornfels (or mafic volcanic) with K-feldspar alteration | |||
| D18-08 | Copper Mountain - Similkameen | T Richards? | K-feldspar-epidote altered mafic volcanic? | similar to D18-06; host rock obscured by strong alteration; K-spar - epidote-albite veins comprise most of sample; white feldspar (2-4 mm) within K-spar areas resemble relict primary plagioclase but are most likely albite alteration; minor biotite and quartz within K-spar; no bornite or other sulphides | |||
| D18-07 | Copper Mountain - Similkameen | Hydrothermal K-feldspar vein | Andesite wallrock to 6 cm wide vein of pink K-feldspar, biotite, quartz, epidote and interstitial calcite | ||||
| D18-06 | Copper Mountain - Similkameen | T Richards? | K-feldspar-epidote altered mafic volcanic? | green and pink; pervasive epidote alteration cross-cut by K-feldspar veins with chlorite envelope; minor euhedral biotite within K-feldspar; specularite(?) crystals widely disseminated within K-feldspar | |||
| D18-05 | Copper Mountain - Similkameen | T Richards? | Fractured sericite-altered rhyolite? | light grey; very fine grained; similar to D18-4 but less siliceous due to sericite and possible chlorite; strong cross-cutting fractures; minor py; one speck cpy; 1-2 cm calcite vein | |||
| D18-04 | Copper Mountain - Similkameen | T Richards? | Rhyolite? | light grey; very fine grained; siliceous; hint of breccia texture; narrow (1-2 mm) silica veinlets | |||
| D18-03 | Copper Mountain - Similkameen | T Richards? | Biotite hornfelsed siltstone | dark purply-brown; bedded; very fine grained; chlorite as patches and irregular, discontinuous veinlets with bleached envelopes | |||
| D18-02 | Copper Mountain - Similkameen | T Richards? | Basalt | dark green-black; very fine grained; non-magnetic; 10% coarse (5 mm) pyrite, fracture-controlled accompanied by minor quartz; black colour may be due to secondary biotite | |||
| D18-01 | Copper Mountain - Similkameen | T Richards? | Mafic volcanic | dark green; massive; fragmental texture is weakly visible, possibly due to hornfels overprint | |||
| D17-08 | Silver Standard | Galena vein | late Cretaceous | fine grained, bleached siltstone with disseminated pyrite and arsenopyrite(?); coarse galena fills vein opening | |||
| D17-07 | Silver Standard | Massive sulphide ore breccia | late Cretaceous | siltstone breccia healed by (in sequential order) carbonate that rims fragments, sphalerite and chalcopyrite, and finally galena and arsenopyrite | |||
| D17-06 | Silver Standard | Siltstone hornfels | laminated; indurated; partly baked because fractures predominate over bedding | ||||
| D17-05 | Silver Standard | Felsite dike | late Cretaceous | bleached quartz-biotite porphyry; fine sericite alteration; disseminated pyrite | |||
| D17-04 | Silver Standard | Carbonaceous sandstone | Jurassic | black; medium grained; unaltered | |||
| D17-03 | Silver Standard | Quartz-siderite cemented breccia | late Cretaceous | fragments all uniformly bleaced siltstone | |||
| D17-02 | Silver Standard | Bleached siltstone | late Cretaceous | light grey; fine grained; massive | |||
| D17-01 | Silver Standard | Siderite cemented breccia | late Cretaceous | angular breccia fragments uniformly bleached; no reaction between ore fluid and wallrock | |||
| D16-09 | Carlin Gold deposits | Manhattan pit | Siltstone (or volcanic) with quartz stockwork | ore grade | |||
| D16-08 | Carlin Gold deposits | Bald Mountain pit | Siltstone with quartz veins | pink, hematitic siltstone, finely laminated; cut by vuggy quartz veins | |||
| D16-07 | Carlin Gold deposits | Gold Quarry | Jasperoid breccia | open space between breccia clasts | |||
| D16-06 | Carlin Gold deposits | Carlin Mine | Bleached limey siltstone | finely laminated; assays to 1 oz/t Au | |||
| D16-05 | Carlin Gold deposits | Carlin Mine | Bleached limey siltstone | finely laminated; assays 1-2 oz/t Au | |||
| D16-04 | Carlin Gold deposits | Carlin Mine | Jasperoid with fine barite | grey, vuggy silica; barite reported but cannot be identified in sample, too fine grained; assays to 0.2 oz/t Au | |||
| D16-03 | Carlin Gold deposits | Carlin Mine | Brecciated jasperoid vein | angular clasts in dark grey silicic matrix; limonite gossan from surface weathering | |||
| D16-02 | Carlin Gold deposits | Gold Quarry | Chert and limey siltstone | purple-black chert in tectonic contact with light grey limey siltstone; assaysto 0.1 oz/t Au | |||
| D16-01 | Carlin Gold deposits | Carlin Mine | Jasperoid vein in shear zone | grey; fine grained siltstone; hard, siliceous; strongly fractured, crackled; gossan weather surface; assays up to 1 oz/t Au | |||
| D14-16 | Bell Copper | 30% coarse grained tarnished pyrite vein with trace qtz + calcite. 60% bleached biotite feldspar porphyry? Strong argillic alteration. | |||||
| D14-15 | Bell Copper | Biotite feldspar porphyry, altered and stockwork veined | Eocene | pervasive hydrothermal biotite in host rock which is poorly visible; stockwork of quartz-pyrite-chalcopyrite veins with K-feldspar envelope and retrograde chlorite-carbonate alteration; calcite on most fracture surfaces | |||
| D14-14 | Bell Copper | Quartz stockwork | Eocene | 90% quartz-pyrite veins; 10% fragments with faintly visible intrusive texture but completely altered to powdery kaolinite | |||
| D14-13 | Bell Copper | Weathered massive chalcopyrite | Eocene | ||||
| D14-12 | Bell Copper | Chalcopyrite vein | Eocene | poor specimen; unrecognizeable wallrock; late coarse calcite |
Samples in your order cart
| Library No. | Suite Name | Location | Collector | Rock Name | Age | Description | Cart |
|---|---|---|---|---|---|---|---|
| A5 04 | Argillic Alteration | T Richards | Argillic spheroidal rhyolite | strong pervasive argillic alteration likely due to steam in a geothermal field; 10% spherules are mostly leached out to voids, some remaining silica and clay; iron oxidized to hematite; strong gossan weathering | |||
| D14-13 | Bell Copper | Weathered massive chalcopyrite | Eocene | ||||
| D14-14 | Bell Copper | Quartz stockwork | Eocene | 90% quartz-pyrite veins; 10% fragments with faintly visible intrusive texture but completely altered to powdery kaolinite | |||
| A5 02 | Argillic Alteration | T Richards | Bladed feldspar porphyry andesite | 30% plagioclase laths, 1-2 cm long, pale green in colour due to sausserite (zoisite / epidote) alteration; microcrystalline groundmass is dark green, likely chlorite altered | |||
| D4-07 | Afton Mines - Ajax suite | Ajax West | Mine staff | Hybrid diorite (microdiorite) | Up Triassic | fine to medium grained, grey-green; equal proportion of chloritized mafics and plagioclase; minor py and epidote | |
| D2-05 | Premier Mine | 2-level portal | D Alldrick | Semi-massive sulphide | Jurassic | 50% py, 20% sph, 1% cpy; quartz and calcite gangue | |
| D14-16 | Bell Copper | 30% coarse grained tarnished pyrite vein with trace qtz + calcite. 60% bleached biotite feldspar porphyry? Strong argillic alteration. | |||||
| A4 11 | Copper-Bearing Propylites | T Richards | Actinolite - quartz skarn breccia | dense, medium grained, prismatic actinolite with 10% rounded quartz "pebbles" that are linked by quartz-chalcopyrite stringers |


