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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Limonite from
Roddick claim, Siwash Creek, Kamloops Mining Division, British Columbia, Canada


Locality type:Claim
Classification
Species:'Limonite' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Limonite data
Locality Data:Click here to view Roddick claim, Siwash Creek, Kamloops Mining Division, British Columbia, Canada
Data Identifiers
Mindat Occurrence Record ID:633672
Long-form Identifier:1:3:633672:1
GUID (UUID V4):0
Nearest other occurrences of Limonite
0.5km (0.3 miles) ⓘMount Baker and Yale Mining Company, Siwash Creek, Kamloops Mining Division, British Columbia, Canada
25.9km (16.1 miles) ⓘPlacer Deposits, Tulameen River, Similkameen Mining Division, British Columbia, Canada
27.2km (16.9 miles) ⓘTreasure Mountain, Tulameen River Area, Similkameen Mining Division, British Columbia, Canada
31.2km (19.4 miles) ⓘEureka-Victoria Silver Mine, Hope, New Westminster Mining Division, British Columbia, Canada
44.9km (27.9 miles) ⓘRainbow prospect, Sumallo River, New Westminster Mining Division, British Columbia, Canada
51.5km (32.0 miles) ⓘGiant Copper deposit, New Westminster Mining Division, British Columbia, Canada
59.3km (36.9 miles) ⓘSiwash Creek, Kamloops Mining Division, British Columbia, Canada
61.1km (38.0 miles) ⓘPlacer Deposits, Similkameen River, Similkameen Mining Division, British Columbia, Canada
62.9km (39.1 miles) ⓘCopper Mountain Mine, Copper Mountain, Princeton, Similkameen Mining Division, British Columbia, Canada
66.2km (41.1 miles) ⓘPrimer porphyry copper prospect, Missezula Lake, Similkameen Mining Division, British Columbia, Canada
References
Geological Survey of Canada (1912) Summary report of the Geological survey branch of the department of mines for 1911 Sessional Paper No. 26.
 
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