Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Magnetite from
Brenda Mine, Peachland, Osoyoos Mining Division, British Columbia, Canada


Locality type:Mine
Classification
Species:Magnetite
Formula:Fe2+Fe23+O4
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Magnetite data
Locality Data:Click here to view Brenda Mine, Peachland, Osoyoos Mining Division, British Columbia, Canada
Data Identifiers
Mindat Occurrence Record ID:623698
Long-form Identifier:1:3:623698:4
GUID (UUID V4):0
Nearest other occurrences of Magnetite
35.8km (22.3 miles) ⓘPrimer porphyry copper prospect, Missezula Lake, Similkameen Mining Division, British Columbia, Canada
54.4km (33.8 miles) ⓘCrystal Peak (Mount Riordan) garnet deposit, Apex Mountain, Osoyoos Mining Division, British Columbia, Canada
56.6km (35.2 miles) ⓘPeggy Mine (Hedley Consolidated), Hedley, Osoyoos Mining Division, British Columbia, Canada
57.2km (35.5 miles) ⓘNickel Plate Mine, Hedley, Osoyoos Mining Division, British Columbia, Canada
58.8km (36.6 miles) ⓘBanbury gold mine (Maple Leaf; Pine Knot), Hedley, Osoyoos Mining Division, British Columbia, Canada
60.9km (37.8 miles) ⓘPlacer Deposits, Similkameen River, Similkameen Mining Division, British Columbia, Canada
60.9km (37.8 miles) ⓘGood Hope Mine, Hedley, Osoyoos Mining Division, British Columbia, Canada
61.6km (38.3 miles) ⓘOregon Mine (French Mine), Hedley, Osoyoos Mining Division, British Columbia, Canada
62.8km (39.0 miles) ⓘLockie Creek, Tulameen, Similkameen Mining Division, British Columbia, Canada
67.7km (42.1 miles) ⓘLucky Mike tungsten occurrence, Swakum Mountain, Merritt area, Nicola Mining Division, British Columbia, Canada
References
Singer, D.A., Berger, V.I., Moring, B.C. (2008) Porphyry copper deposits of the world: Database and grade and tonnage models, 2008. Open-File Report 2008-1155
 
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