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 |
---|---|---|---|---|---|---|---|
T6-06 | Epithermal Gold-Silver veins | Lawyers, Toodoggone | D Lefebure | Brecciated feldspar porphyry with quartz veins | Jurassic | multiple episodes of quartz veins; veins are banded to coxcomb texture | |
T6-05 | Epithermal Gold-Silver veins | Lawyers, Toodoggone | D Lefebure | Banded quartz vein in tuff | Jurassic | symmetrically banded, 1.5 cm chalcedonic quartz vein in pinkish-brown tuff; core of vein has some crystalline quartz with hint of amythest colour | |
T6-04 | Epithermal Gold-Silver veins | Lawyers, Toodoggone | D Lefebure | Plagioclase phyric tuff | Jurassic | layered; pink feldspar in reddish grounmass; feldspar in crystal-rich beds; feldspar is likely hematitized plagioclase, crystals do not resemble primary K-feldspar | |
T6-03 | Epithermal Gold-Silver veins | Lawyers, Toodoggone | D Lefebure | Dacite tuff | Jurassic | light brown; 10% plagioclase crystals, 1 mm size, orange in colour due to cloudy hematite; groundmass has pervasive chlorite (propylitic alteration) | |
T6-02 | Epithermal Gold-Silver veins | Al prospect, Toodoggone | D Lefebure | Quartz | Jurassic | white; drusy, minor open space; vein or silicified rock? | |
T6-01 | Epithermal Gold-Silver veins | Al prospect, Toodoggone | D Lefebure | Clay-alunite alteration | Jurassic | white; massive; fine grained; light density; bladed crystals evident on one weathered surface | |
T5-12 | Skarn | Epidote-calcite skarn | parent rock is andesite with abundant secondary calcite | ||||
T5-11 | Skarn | French Mine, Hedley | Biotite hornfels argillite | dark purplish-brown; very fine grained; colour indicates pervasive metamorphic biotite | |||
T5-10 | Skarn | French Mine, Hedley | K-feldspar-epidote-chalcopyrite skarn | 40% K-feldspar; 40% epidote; 15% chalcopyrite | |||
T5-09 | Skarn | Nickel Plate mine, Hedley | Quartz-eye rhyolite dike | very pale grey; massive; aphanitic; 3-4% quartz phenocrysts; trace arsenopyrite | |||
T5-08 | Skarn | Nickel Plate mine, Hedley | Sulphide skarn | 75% pyrrhotite; 10% chalcopyrite; 10% pyrite; 5% arsenopyrite | |||
T5-07 | Skarn | Hedley | Copperfield conglomerate marker horizon | cobbles to 8 cm; biotite hornfels of argillaceous matrix; composition is wrong to develop skarn | |||
T5-06 | Skarn | French Mine, Hedley | Diorite | dark grey-green; fine-medium grained; 25% hornblende; 75% indistinguishable feldspathic groundmass | |||
T5-05 | Skarn | Blue Grouse, Vancouver Is. | Feldspar porphyry diorite | green; medium grained; 60% feldspar; 25% hornblende; intrusion responsible for skarn development | |||
T5-04 | Skarn | Blue Grouse, Vancouver Is. | Garnet-epidote-actinolite skarn | 40% epidote; 25% garnet; 25% actinolite; 10% quartz | |||
T5-03 | Skarn | Bob deposit, Banks Island | Arsenopyrite skarn | 50% quartz; 30% arsenopyrite; 10% sphalerite; 5% chalcopyrite | |||
T5-02 | Skarn | French Mine, Hedley | Garnet skarn | 85% pink-brown garnet; 5% pyroxene; 5% quartz; 5-10% calcite | |||
T5-01 | Skarn | Tasu | Magnetite skarn | Triassic | 95% magnetite; 5% pyrite plus chalcopyrite | ||
T4-11 | Skarn | Blue Grouse, Vancouver Is. | Garnet-epidote skarn | one rock cut in two, one half with no label; brown weathered makes minerals garnet and epidote difficult to recognize; 15% interstitial calcite | |||
T4-10 | Skarn | French mine, Hedley | Magnetite skarn | 95% magnetite; 5% pyrite plus chalcopyrite | |||
T4-09 | Skarn | Nickel Plate, Hedley | Sulphide skarn | coarse grained; massive; 40% arsenopyrite; 30% pyrite; 20% pyrrhotite; 10% chalcopyrite | |||
T4-08 | Skarn | French mine, Hedley | Pyroxene-bornite skarn | dense; fine grained; 10% bornite; 1% chalcopyrite | |||
T4-07 | Skarn | Blue Grouse, Vancouver Is. | Diorite | same rock as in C2 | |||
T4-06 | Skarn | French mine, Hedley | Garnet-calcite skarn | 25% garnet | |||
C1 05 (missing) | Skarn | French mine, Hedley | |||||
T4-04 | Skarn | Bob deposit, Banks Island | Hornblende granodiorite | 85% feldspar (predominantly plagioclase, no K-feldspar observed); 10% hornblende; <1% biotite | |||
T4-03 | Skarn | Bob deposit, Banks Island | Sulphide skarn | 70% arsenopyrite; 10% sphalerite; 5% pyrite; 15% quartz; reported to contain 0.59 oz/t Au, 0.29 oz/t Ag, 9.98% Zn | |||
T4-02 | Skarn | Bob deposit, Banks Island | Garnet skarn | 90% garnet; 2% pyroxene; 6% calcite | |||
T4-01 | Skarn | Tasu | Magnetite skarn | Triassic | 95% magnetite; 5% pyrite plus chalcopyrite; same as C2 01 | ||
T3-11 | Manto & Sedex | Mudstone with barite laminae | Devonian | white barite as fine laminations, <1 mm thick in black mudstone | |||
T3-10 | Manto & Sedex | Sullivan | Bedded pyrite-pyrrhotite in shale | Proterozoic | same as B1 07 | ||
T3-09 | Manto & Sedex | Cirque | Massive barite | Devonian | crudely bedded; bedding disrupted; recrystallized barite; minor galena | ||
T3-08 | Manto & Sedex | Mt. Alcock | Semi-massive barite | Devonian | very fine grained; dense; 5% fine galena (similar to B1 05) | ||
T3-07 | Manto & Sedex | Midway | Massive sulphide | Devonian | 70% pyrite; 20% galena; 5% sphalerite; not bedded | ||
B2 01 (missing) | Manto & Sedex | Midway | Bedded shale | Devonian | |||
T3-06 | Manto & Sedex | Sullivan | Bedded pyrite-pyrrhotite in shale | Proterozoic | black, 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 | ||
T3-05 | Manto & Sedex | Cirque | Massive sulphide | Devonian | massive pyrite with 6% sphalerite, 1% galena | ||
T3-04 | Manto & Sedex | Mt. Alcock | Massive barite | Devonian | pale grey; disrupted bedding and coarse recrystallization of barite; 3-5% galena seams | ||
T3-03 | Manto & Sedex | Mt. Alcock | Massive sulphide | Devonian | dark 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 & Sedex | Midway | Shale breccia with pyrite-carbonate cement | ||||
T3-02 | Manto & Sedex | Midway | Tectonic shale breccia with sulphide cement | Devonian | identical specimens; brittle breccia healed by coarse pyrite, galena and sphalerite | ||
T3-01 | Manto & Sedex | Midway | Shale with pyrite bed | Devonian | drill core of very thin bedded shale3 cm thick pyrite bed; pyrite is recrystallized into minute cubes | ||
A2 12 (missing) | VMS | Tyee deposit, Mt Sicker, Vancouver Is. | Ferrocrete | Recent | |||
T2-11 | VMS | Lynx deposit, Myra Falls | Kuroko black ore (bedded pyrite-chalcopyrite-sphalerite) | Devonian | 30% sphalerite; 30% pyrite; 10% chalcopyrite; 20% silica gangue | ||
T2-10 | VMS | Lenora Pit, Mt Sicker | Chert with pyrite-chalcopyrite veins | chert is well fractured and broken with in-filling of sulphide veins to 2 cm wide; pyrite to chalcopyrite ration is 10:1 | |||
T2-09 | VMS | HW deposit, Myra Falls | Massive pyritic ore | Devonian | layered but only vaguely bedded; 60% pyrite; 5% chalcopyrite;30% silica (and perhaps barite); no galena seen but likely a few % sphalerite | ||
T2-08 | VMS | Windy Craggy | Chlorite-pyrrhotite tuff | 10% pyrrhotite, finely bedded within massive chlorite, likely a fine tuff or basalt-derived mud; weakly magnetic | |||
T2-07 | VMS | Kutcho | Recrystallized massive pyrite | Lower Triassic | 80% fine to coarse pyrite; the coarse pyrite (to 1 cm) is associated with remobilized chalcopyrite (3%), bornite (3%) and coarse quartz (10%) | ||
T2-06 | VMS | Lenora Pit, Mt Sicker | Chalcopyrite ore | Devonian | 25% 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 | ||
T2-05 | VMS | Tyee deposit, Mt Sicker, Vancouver Is. | Kuroko black ore | Devonian | 60% sphalerite (and galena?); 20% pyrite; 15% barite; <5% calcite as durchbewegung clasts |
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