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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
S16-10Cronin PhyllonitesSlategrey
S16-09Cronin PhyllonitesMicaceous siltstonewell foliated; prominent micaceous component; detrital grains visible
S16-08Cronin PhyllonitesSandstone / quartzitepink
S16-07Cronin PhyllonitesAtna PeakSandstone / quartzitegrey; crinkle folding produces lineation in muscovite
S16-06Cronin PhyllonitesBabine RangeGraphitic black argillitelustrous black; slightly greasy texture suggests graphitic component
S16-05Cronin PhyllonitesBabine RangePhyllitegrey to pink; fine grained; indistinct texture; probably sedimentary origin
S16-04Cronin PhyllonitesBabine RangeLapilli tuff70% purple matrix of intermediate (andesite) composition; 30% angular, aphanitic fragments, mainly felsic, a few green andesite
S16-03Cronin PhyllonitesBabine RangeSiltstonethin bedded,
S16-02Cronin PhyllonitesBabine RangeSiltstonethin bedded (mm to cm); pale grey silt grades up to dark grey argillaceous tops; distal turbidite
S16-01Cronin PhyllonitesBabine RangeBlack argillite
S15-67P SchiarizzaListwanitewhite and green with strong brown iron weathered surface; banded with quartz, iron-carbonate, mariposite; 2-3% disseminated chromite
S15-66P SchiarizzaMercury veincinnabar
S15-65P SchiarizzaMercury veinquartz and cinnabar
S15-64P SchiarizzaStibnite-carbonate veinstibnite is brecciated by carbonate
S15-63P SchiarizzaStibnite-quartz veinbanded quartz and stibnite
S15-62P SchiarizzaPolymetallic veinarsenopyrite; pyrite; sphalerite; galena; non-magnetic pyrrhotite(?)
S15-61P SchiarizzaPolymetallic veinmainly arsenopyrite and quartz; minor pyrrhotite(?), non-magnetic; arsenopyrite is partially altered to grass-green scorodite
S15-60Bralorne IntrusionsP SchiarizzaSodic granitelight grey; 60% feldspar; 30% quartz; 10% hornblende(?), chloritized
S15-59Bralorne IntrusionsP SchiarizzaDioritemedium grained; massive; feldspar partially altered to pale green epidote
S15-58Bralorne IntrusionsP SchiarizzaDioritemedium grained; massive; 75-80% plagioclase; 20-25% hornblende(?) altered to chlorite
S15-57Bralorne IntrusionsP SchiarizzaGabbromedium grained; massive; 40% plagioclase; 60% pyroxene
S15-56Bralorne IntrusionsP SchiarizzaUltramafiteblack to dark green; medium grained; foliated with secondary serpentine; 80% mafic minerals (olivine? Pyroxene?); 10-20% feldspar
S15-55Jackass Mtn GrpP SchiarizzaArkosic wackeLower Cretaceousmottled grey and green; detrital quartz, feldspar and mafics; no bedding, massive
S15-54Jackass Mtn GrpP SchiarizzaSandstone / siltstoneLower Cretaceousmedium grey; well bedded on mm scale
S15-53Jackass Mtn GrpP SchiarizzaGreywackeLower Cretaceousmedium green; 95% of grains are mm size; 5% cm size clasts; includes one granitic clast
S15-52Jackass Mtn GrpP SchiarizzaGreywacke / congomerateLower Cretaceousdark brown; heterolithic; contains limestone clasts
S15-51Jackass Mtn GrpP SchiarizzaLimey sandstone / wackeLower Cretaceousmedium dark grey; fossil remnants?
S15-50Methow BasinP SchiarizzaGreywacke / sandstoneMid Jurassicgreen-brown; well sorted; fine grained, grains < 0.5 mm
S15-49Methow BasinP SchiarizzaGreywackeMid Jurassicsimilar to above, with argillite rip-up clasts to 3 cm
S15-48Methow BasinP SchiarizzaGreywackeMid Jurassicmedium grey; 1-3 mm clasts, sub-round to sub-angular; heterolithic; well sorted; no bedding
S15-47Cadwallader Grp, Hurley FmP SchiarizzaLimey sandstoneLate Triassicgrey; strong acid reaction
S15-46Cadwallader Grp, Hurley FmP SchiarizzaArgilliteLate Triassicpurple-black
S15-45Cadwallader Grp, Hurley FmP SchiarizzaSandstoneLate Triassicgreen-brown; massively bedded
S15-44Cadwallader Grp, Hurley FmP SchiarizzaCoarse sandstoneLate Triassicgreen-grey; clasts 3-4 mm
S15-43Cadwallader Grp, Hurley FmP SchiarizzaChert pebble conglomerateLate Triassic80% pebbles; clast supported
S15-42Cadwallader Grp, Pioneer FmP SchiarizzaDiabaseLate Triassicblack; fine-medium grained; 50% acicular plagioclase laths; 50% acicular hornblende
S15-41Cadwallader Grp, Pioneer FmP SchiarizzaBasaltLate Triassicpurple; 25% feldspar phenocrysts; 5% cavities, leached vesicles?
S15-40Tyaughton GrpP SchiarizzaConglomerateLatest Triassicgrey-brown; clasts to 0.5 cm
S15-39Tyaughton GrpP SchiarizzaSandstone / GreywackeLatest Triassicgrey; coarse; heterolithic
S15-38Tyaughton GrpP Schiarizzaa. Siltstone; b. Wacke; c. ConglomerateLatest Triassicall 3 rocks are distinctive tan brown; conglomerate is heterolithic with 5% chert clasts
S15-37Lost Ck FmP SchiarizzaGreywacke / congomerateLo-Mid Jurassictexture indistinct due to weathered surfaces
S15-36Lost Ck FmP SchiarizzaSiltstoneLo-Mid Jurassicgrey silt; with thin black (organic?) beds; well bedded
S15-35Relay Mtn GrpP SchiarizzaChert pebble conglomerateJura-Cretaceouswell rounded clasts; dark grey matrix; looks to be matrix supported
S15-34Relay Mtn GrpP SchiarizzaSandstoneJura-Cretaceousbrownish-grey; massive (no bedding) missing
S15-33Relay Mtn GrpP SchiarizzaSilty black limestoneJura-Cretaceouscross-bedded; delicately bedded
S15-32Relay Mtn GrpP SchiarizzaArgilliteJura-Cretaceouspurplish black; finely bedded
S15-31Taylor Ck Dash FmP SchiarizzaConglomerateUp Lower Cretaceousheterolithic; mainly 1 cm size pebbles but up to 5 cm cobble
S15-30Taylor Ck Eastern facies, Lizard FmP SchiarizzaVolcanic sandstoneUp Lower Cretaceousvery dark grey; well sorted fine sand, < 1 mm size; detrital mica
S15-29Taylor Ck Eastern facies, Lizard FmP SchiarizzaVolcanic sandstoneUp Lower Cretaceousbrown; well sorted fine sand, < mm size; detrital mica
S15-28Taylor Ck Western faciesP SchiarizzaBasalt epiclastic conglomerateUp Lower Cretaceousclasts and matrix are all derived from basalt

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