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 |
|---|---|---|---|---|---|---|---|
| S21-05 | Skeena | T Richards | Red siltsone to slate | thin bedded; fine grained; gritty texture indicates detrital sand, siltstone, not shale | |||
| S21-04 | Skeena | T Richards | Fine sandstone | dark grey; massive; homogenous | |||
| S21-03 | Skeena | T Richards | Sandstone to siltstone | graded sand to silt in 10 cm thick beds; well bedded; similar greenish colour as above in sand layer grading to grey-black in fine layers | |||
| S21-02 | Skeena | T Richards | Coarse sandstone to conglomerate | massive; same greenish colour as above; round clasts to 1 cm; angular to rounded grains; possibly Smithers Formation? | |||
| S21-01 | Skeena | T Richards | Sandstone | massive, no bedding; homogenous; greenish; subround grains | |||
| S19-27 | Atlin | Anderson Bay, Anderson Bay basalt | M A Bloodgood | Olivine basalt | locally columnar | ||
| S19-26 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Lapilli tuff | fine grained ash matrix | ||
| S19-25 | Atlin | Cache Creek Group, Sentinel Mountain | M A Bloodgood | Banded chert | contains radiolarian fossils | ||
| S19-24 | Atlin | Cache Creek Group, Sentinel Mountain | M A Bloodgood | Banded chert | red and green bands | ||
| S19-23 | Atlin | Sentinel Mountain, west flank | M A Bloodgood | Tectonized volcanic sediments | chert pebbles | ||
| S19-22 | Atlin | Laberge Group, Atlin Lk | M A Bloodgood | sandstone | quartz-rich | ||
| S19-21 | Atlin | Anderson Bay, Anderson Bay basalt | M A Bloodgood | Olivine basalt | locally columnar | ||
| S19-20 | Atlin | Cache Creek Group, Sentinel Mountain, north of head of Eldorado Creek | M A Bloodgood | Mylonitized gabbro | mineral lineation on top surface near tape label | ||
| S19-19 | Atlin | M A Bloodgood | Conglomerate | immature; rounded to very angular clasts | |||
| S19-18 | Atlin | Mt McCallum | M A Bloodgood | Rhyolite dike | cuts Sloko volcanics | ||
| S19-17 | Atlin | Sentinel Mountain, unnamed stratigraphic unit | M A Bloodgood | Triassic | calcareous; gritty sandstone; interbedded limestone has Norian conodonts | ||
| S19-16 | Atlin | M A Bloodgood | Granite pebble conglomerate | greywacke matrix; matrix supported | |||
| S19-15 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Andesite dike | plagioclase and amphibole phyric; dike cuts Group A | ||
| S19-14 | Atlin | Cache Creek Group, Sentinel Mountain | M A Bloodgood | Amygdaloidal basalt | |||
| S19-13 | Atlin | M A Bloodgood | Greywacke | ||||
| S19-12 | Atlin | Sloko Group, ridge west of Atlin Mountain | M A Bloodgood | Pebble conglomerate | |||
| S19-11 | Atlin | Sloko Group, ridge west of Atlin Mountain | M A Bloodgood | Conglomerate | lithic ash tuff clasts | ||
| S19-10 | Atlin | Sloko Group, ridge west of Atlin Mountain | M A Bloodgood | Sandstone | |||
| S19-09 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Conglomerate | plagioclase porphyry clasts | ||
| S19-08 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Volcanic sandstone | fine grained | ||
| S19-07 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Tuff | laminated bed within volcanic breccia | ||
| S19-06 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Ash tuff | laminated; siliceous | ||
| S19-05 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Lapilli tuff | fine grained ash matrix | ||
| S19-04 | Atlin | Group A, Atlin Mountain | M A Bloodgood | Ash tuff | well bedded | ||
| S19-03 | Atlin | Fourth of July batholith, west shore of Atlin Lk, Safety Cove | M A Bloodgood | K-feldspar megacrystic granite | |||
| S19-02 | Atlin | Fourth of July batholith, west shore of Atlin Lk, Safety Cove | M A Bloodgood | Hornblende biotite granite | |||
| S19-01 | Atlin | M A Bloodgood | Greenstone mylonite | dark grey-green; strong fabric; limestone augen | |||
| S18-56 | Edziza Volcano | Pyramid Fm | J Souther | Sanidine porphyry trachyte | Cenozoic | 65-70% light grey matrix; 25-30% coarse sanidine to 1 cm; 5% pyroxene, 1-3 mm size | |
| S18-55 | Edziza Volcano | Pyramid Fm | J Souther | Airfall lapilli tuff | Cenozoic | very pale grey; heterolithic; clasts to 1 cm; low density; no welding or flow texture | |
| S18-54 | Edziza Volcano | Pyramid Fm | J Souther | Spherulitic ash flow | Cenozoic | tight flow fold in strongly banded ash flow | |
| S18-53 | Edziza Volcano | Pyramid Fm | J Souther | Spherulitic rhyolite | Cenozoic | 25% concentric spherules, up to 1-2 cm diameter, pinish colour; 5% smaller (0.4 cm) white spherules commonly with black rim; 70% matrix that is grey and aphanitic surrounding the spherules and grades to finely crystalline late filling of the interstitial areas | |
| S18-52 | Edziza Volcano | Pyramid Fm | J Souther | Obsidian | Cenozoic | black obsidian; minor streaky siliceous laminae (devitrification) | |
| S18-51 | Edziza Volcano | Pyramid Fm | J Souther | Intermixed glaciofluvial gravel and obsidian | Cenozoic | ||
| S18-50 | Edziza Volcano | Pyramid Fm | J Souther | Volcanic glass | Cenozoic | interlayered glass and devitrified glass, interlayered on mm to cm scale | |
| S18-49 | Edziza Volcano | Armadillo Fm | J Souther | Breccia, hydrothermally altered | Miocene | 40% pale green matrix, mainly silica; 40% heterolithic clasts, leached, altered with 10% void space; probably hydrothermal vent breccia | |
| S18-48 | Edziza Volcano | Armadillo Fm | J Souther | Felsic lapilli tuff | Miocene | grey; heterolithic; clasts to 3 cm, most are 5 mm or less; classts are white grey, some are welded, one is obsidian; some clasta are outlined by a black rim of ?? Unknown | |
| S18-47 | Edziza Volcano | Armadillo Fm | J Souther | Felsic ash tuff | Miocene | layered, alternating finely vesicular bands; 5% clasts, <1 mm size | |
| S18-46 | Edziza Volcano | Armadillo Fm | J Souther | Basalt? | Miocene | grey (too felsic for basalt?); 5-10% olivine(?); 3-4% plagioclase laths; 1% hornblende needles | |
| S18-45 | Edziza Volcano | Armadillo Fm | J Souther | Felsic tuff | Miocene | pale brown matrix; 10-20% heterolithic clasts, <1 mm size, grey, red, other shades | |
| S18-44 | Edziza Volcano | Armadillo Fm | J Souther | Feldspar crystal-lithic ash flow tuff | Miocene | black and pale orange-brown; strongly flow-aligned texture; 5% feldspar, 1-3 mm size; 10% lithic clasts to 2 cm | |
| S18-43 | Edziza Volcano | Armadillo Fm | J Souther | Obsidian | Miocene | black rhyolite glass; 20% silica spherules, uniform 2 mm size | |
| S18-42 | Edziza Volcano | Armadillo Fm | J Souther | Felsic tuff | Miocene | grey; finely laminated with white mm layers; one layer with unknown black crystal pseudomorphs, few mm in size | |
| S18-41 | Edziza Volcano | Armadillo Fm | J Souther | Rhyolite ash flow | Miocene | light coloured; densely packed clasts, angular to rounded, mainly 0.5 cm but up to 1 cm; clasts are various shades of white and light to dark grey; locally welded texture | |
| S18-40 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | 3-4% olivine; 3-4% feldspar; sparse calcite amygdules, 1 mm size | |
| S18-39 | Edziza Volcano | Raspberry Fm | J Souther | Basalt | Cenozoic | 5% feldspar and amygdules, sub-mm size; most are amygdules of chalcedony and calcite, feldspars indicated by crystal shape |
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 |


