• Site banners
  • Site banners

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:

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 NameLocationCollectorRock NameAgeDescriptionCart
S21-05SkeenaT RichardsRed siltsone to slatethin bedded; fine grained; gritty texture indicates detrital sand, siltstone, not shale
S21-04SkeenaT RichardsFine sandstonedark grey; massive; homogenous
S21-03SkeenaT RichardsSandstone to siltstonegraded 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
S21-02SkeenaT RichardsCoarse sandstone to conglomeratemassive; same greenish colour as above; round clasts to 1 cm; angular to rounded grains; possibly Smithers Formation?
S21-01SkeenaT RichardsSandstonemassive, no bedding; homogenous; greenish; subround grains
S19-27AtlinAnderson Bay, Anderson Bay basaltM A BloodgoodOlivine basaltlocally columnar
S19-26AtlinGroup A, Atlin MountainM A BloodgoodLapilli tufffine grained ash matrix
S19-25AtlinCache Creek Group, Sentinel MountainM A BloodgoodBanded chertcontains radiolarian fossils
S19-24AtlinCache Creek Group, Sentinel MountainM A BloodgoodBanded chertred and green bands
S19-23AtlinSentinel Mountain, west flankM A BloodgoodTectonized volcanic sedimentschert pebbles
S19-22AtlinLaberge Group, Atlin LkM A Bloodgoodsandstonequartz-rich
S19-21AtlinAnderson Bay, Anderson Bay basaltM A BloodgoodOlivine basaltlocally columnar
S19-20AtlinCache Creek Group, Sentinel Mountain, north of head of Eldorado CreekM A BloodgoodMylonitized gabbromineral lineation on top surface near tape label
S19-19AtlinM A BloodgoodConglomerateimmature; rounded to very angular clasts
S19-18AtlinMt McCallumM A BloodgoodRhyolite dikecuts Sloko volcanics
S19-17AtlinSentinel Mountain, unnamed stratigraphic unitM A BloodgoodTriassiccalcareous; gritty sandstone; interbedded limestone has Norian conodonts
S19-16AtlinM A BloodgoodGranite pebble conglomerategreywacke matrix; matrix supported
S19-15AtlinGroup A, Atlin MountainM A BloodgoodAndesite dikeplagioclase and amphibole phyric; dike cuts Group A
S19-14AtlinCache Creek Group, Sentinel MountainM A BloodgoodAmygdaloidal basalt
S19-13AtlinM A BloodgoodGreywacke
S19-12AtlinSloko Group, ridge west of Atlin MountainM A BloodgoodPebble conglomerate
S19-11AtlinSloko Group, ridge west of Atlin MountainM A BloodgoodConglomeratelithic ash tuff clasts
S19-10AtlinSloko Group, ridge west of Atlin MountainM A BloodgoodSandstone
S19-09AtlinGroup A, Atlin MountainM A BloodgoodConglomerateplagioclase porphyry clasts
S19-08AtlinGroup A, Atlin MountainM A BloodgoodVolcanic sandstonefine grained
S19-07AtlinGroup A, Atlin MountainM A BloodgoodTufflaminated bed within volcanic breccia
S19-06AtlinGroup A, Atlin MountainM A BloodgoodAsh tufflaminated; siliceous
S19-05AtlinGroup A, Atlin MountainM A BloodgoodLapilli tufffine grained ash matrix
S19-04AtlinGroup A, Atlin MountainM A BloodgoodAsh tuffwell bedded
S19-03AtlinFourth of July batholith, west shore of Atlin Lk, Safety CoveM A BloodgoodK-feldspar megacrystic granite
S19-02AtlinFourth of July batholith, west shore of Atlin Lk, Safety CoveM A BloodgoodHornblende biotite granite
S19-01AtlinM A BloodgoodGreenstone mylonitedark grey-green; strong fabric; limestone augen
S18-56Edziza VolcanoPyramid FmJ SoutherSanidine porphyry trachyteCenozoic65-70% light grey matrix; 25-30% coarse sanidine to 1 cm; 5% pyroxene, 1-3 mm size
S18-55Edziza VolcanoPyramid FmJ SoutherAirfall lapilli tuffCenozoicvery pale grey; heterolithic; clasts to 1 cm; low density; no welding or flow texture
S18-54Edziza VolcanoPyramid FmJ SoutherSpherulitic ash flowCenozoictight flow fold in strongly banded ash flow
S18-53Edziza VolcanoPyramid FmJ SoutherSpherulitic rhyoliteCenozoic25% 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
S18-52Edziza VolcanoPyramid FmJ SoutherObsidianCenozoicblack obsidian; minor streaky siliceous laminae (devitrification)
S18-51Edziza VolcanoPyramid FmJ SoutherIntermixed glaciofluvial gravel and obsidianCenozoic
S18-50Edziza VolcanoPyramid FmJ SoutherVolcanic glassCenozoicinterlayered glass and devitrified glass, interlayered on mm to cm scale
S18-49Edziza VolcanoArmadillo FmJ SoutherBreccia, hydrothermally alteredMiocene40% pale green matrix, mainly silica; 40% heterolithic clasts, leached, altered with 10% void space; probably hydrothermal vent breccia
S18-48Edziza VolcanoArmadillo FmJ SoutherFelsic lapilli tuffMiocenegrey; 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
S18-47Edziza VolcanoArmadillo FmJ SoutherFelsic ash tuffMiocenelayered, alternating finely vesicular bands; 5% clasts, <1 mm size
S18-46Edziza VolcanoArmadillo FmJ SoutherBasalt?Miocenegrey (too felsic for basalt?); 5-10% olivine(?); 3-4% plagioclase laths; 1% hornblende needles
S18-45Edziza VolcanoArmadillo FmJ SoutherFelsic tuffMiocenepale brown matrix; 10-20% heterolithic clasts, <1 mm size, grey, red, other shades
S18-44Edziza VolcanoArmadillo FmJ SoutherFeldspar crystal-lithic ash flow tuffMioceneblack and pale orange-brown; strongly flow-aligned texture; 5% feldspar, 1-3 mm size; 10% lithic clasts to 2 cm
S18-43Edziza VolcanoArmadillo FmJ SoutherObsidianMioceneblack rhyolite glass; 20% silica spherules, uniform 2 mm size
S18-42Edziza VolcanoArmadillo FmJ SoutherFelsic tuffMiocenegrey; finely laminated with white mm layers; one layer with unknown black crystal pseudomorphs, few mm in size
S18-41Edziza VolcanoArmadillo FmJ SoutherRhyolite ash flowMiocenelight 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
S18-40Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoic3-4% olivine; 3-4% feldspar; sparse calcite amygdules, 1 mm size
S18-39Edziza VolcanoRaspberry FmJ SoutherBasaltCenozoic5% 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 NameLocationCollectorRock NameAgeDescriptionCart
A5 04Argillic AlterationT RichardsArgillic spheroidal rhyolitestrong 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
D14-13Bell CopperWeathered massive chalcopyriteEocene
D14-14Bell CopperQuartz stockworkEocene90% quartz-pyrite veins; 10% fragments with faintly visible intrusive texture but completely altered to powdery kaolinite
A5 02Argillic AlterationT RichardsBladed feldspar porphyry andesite30% plagioclase laths, 1-2 cm long, pale green in colour due to sausserite (zoisite / epidote) alteration; microcrystalline groundmass is dark green, likely chlorite altered
D4-07Afton Mines - Ajax suiteAjax WestMine staffHybrid diorite (microdiorite)Up Triassicfine to medium grained, grey-green; equal proportion of chloritized mafics and plagioclase; minor py and epidote
D2-05Premier Mine2-level portalD AlldrickSemi-massive sulphideJurassic50% py, 20% sph, 1% cpy; quartz and calcite gangue
D14-16Bell Copper30% coarse grained tarnished pyrite vein with trace qtz + calcite. 60% bleached biotite feldspar porphyry? Strong argillic alteration.
A4 11Copper-Bearing PropylitesT RichardsActinolite - quartz skarn brecciadense, medium grained, prismatic actinolite with 10% rounded quartz "pebbles" that are linked by quartz-chalcopyrite stringers
Order your samples and book a viewing time.

Want to help SEG keep the Rock Room going? Donate using the button below.