Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Hematite from
Nottingham Mine (Nottingham deposit; Clear Hills Prospect), Wee Jasper, Buccleuch Co., New South Wales, Australia


Locality type:Mine
Classification
Species:Hematite
Formula:Fe2O3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Hematite data
Locality Data:Click here to view Nottingham Mine (Nottingham deposit; Clear Hills Prospect), Wee Jasper, Buccleuch Co., New South Wales, Australia
Data Identifiers
Mindat Occurrence Record ID:1349037
Long-form Identifier:1:3:1349037:3
GUID (UUID V4):0
Nearest other occurrences of Hematite
12.0km (7.4 miles) ⓘGlen deposit (The Glen; The Glen mine), Wee Jasper, Buccleuch Co., New South Wales, Australia
27.7km (17.2 miles) ⓘPaddy's River Mine, Paddy's River District, Australian Capital Territory, Australia
29.0km (18.1 miles) ⓘPaddy's River Iron prospect, Paddy's River District, Australian Capital Territory, Australia
38.7km (24.1 miles) ⓘGooda Creek Gold prospect, Murray Co., New South Wales, Australia
48.7km (30.3 miles) ⓘBasin Creek Copper Prospect, Tumut, Wynyard Co., New South Wales, Australia
51.1km (31.8 miles) ⓘBlack Maria Gold Mine, Murray Co., New South Wales, Australia
52.2km (32.5 miles) ⓘGarnet Hill, Yarrangobilly, Buccleuch Co., New South Wales, Australia
69.3km (43.0 miles) ⓘMargarets Creek prospect (Iron Pit zone), Michelago, Beresford Co., New South Wales, Australia
69.4km (43.1 miles) ⓘHoskins Iron and Steel Co Ltd deposit (Margarets Creek prospect), Michelago, Beresford Co., New South Wales, Australia
73.1km (45.5 miles) ⓘMichelago Iron Quarries (Kellyville prospect), Beresford Co., New South Wales, Australia
References
Gilligan, L.B. (1975) Part 1. Mine Data Sheets to accompany Metallogenic Map, Canberra 1:250 000 Sheet. Geological Survey of New South Wales, Department of Mines.
 
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