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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Siltstone from
Mt Everest Copper Mine, Upper Bingara, Murchison Co., New South Wales, Australia


Locality type:Mine
Classification
Type:Siltstone
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Siltstone data
Locality Data:Click here to view Mt Everest Copper Mine, Upper Bingara, Murchison Co., New South Wales, Australia
Data Identifiers
Mindat Occurrence Record ID:1206293
Long-form Identifier:1:3:1206293:3
GUID (UUID V4):0
Nearest other occurrences of Siltstone
0.4km (0.3 miles) ⓘWithers Mine, Upper Bingara, Murchison Co., New South Wales, Australia
16.1km (10.0 miles) ⓘMurchison Copper Mine (Murchison lode; Piedmont Mine; Cooks Mine), Gulf Creek, Upper Bingara, Murchison Co., New South Wales, Australia
16.7km (10.4 miles) ⓘOaky Creek Stibnite deposit, Cobbadah, Murchison Co., New South Wales, Australia
17.9km (11.1 miles) ⓘGulf Creek Copper Mine (Cornish Copper Mine), Gulf Creek, Upper Bingara, Murchison Co., New South Wales, Australia
18.0km (11.2 miles) ⓘGulf Creek Mine (Gulf Creek Copper Mine), Gulf Creek, Upper Bingara, Murchison Co., New South Wales, Australia
26.4km (16.4 miles) ⓘCaroda magnetite, Caroda, Murchison Co., New South Wales, Australia
30.0km (18.6 miles) ⓘGardiners Diatomite deposit, Barraba, Darling Co., New South Wales, Australia
30.6km (19.0 miles) ⓘMcGuinness Clay deposit, Barraba, Darling Co., New South Wales, Australia
32.0km (19.9 miles) ⓘGoldmans deposit, Barraba, Darling Co., New South Wales, Australia
32.5km (20.2 miles) ⓘJunior Mine (Spencers Manganese Mine), Barraba, Darling Co., New South Wales, Australia
References
Brown, R.E.; Brownlow, J.W.; Krynen, J.P. (1992) Metallogenic Study and Mineral Deposit Data Sheets, Manilla-Narrabri 1:250 000 Metallogenic Map SH/56-9, SH/55-12. Geological Survey of New South Wales.
 
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