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Cassiterite from
Couchs lode, Stannum, Gough Co., New South Wales, Australia


Locality type:Lode
Classification
Species:Cassiterite
Formula:SnO2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Cassiterite data
Locality Data:Click here to view Couchs lode, Stannum, Gough Co., New South Wales, Australia
Data Identifiers
Mindat Occurrence Record ID:698145
Long-form Identifier:1:3:698145:7
GUID (UUID V4):62281b9e-3146-4e43-90fe-438863fc14de
Nearest other occurrences of Cassiterite
0.2km (0.1 miles) Castle Wellington Mine, Stannum, Gough Co., New South Wales, Australia
0.2km (0.2 miles) Pinchgut deposit, Stannum, Gough Co., New South Wales, Australia
0.5km (0.3 miles) Curnows Stannum lode, Stannum, Gough Co., New South Wales, Australia
0.9km (0.5 miles) Folkstone lode, Stannum, Gough Co., New South Wales, Australia
1.1km (0.7 miles) Nine Mile Creek (Gunns Gully; Middle Swamp; Robertsons Creek; Interstate deposit), Stannum, Gough Co., New South Wales, Australia
1.4km (0.8 miles) Brown and party deposit, Stannum, Gough Co., New South Wales, Australia
1.5km (0.9 miles) Browns alluvials, Stannum, Gough Co., New South Wales, Australia
1.5km (1.0 miles) Cemetery lode, Stannum, Gough Co., New South Wales, Australia
1.6km (1.0 miles) Wet Flat (Nine Mile lead; Jeremys Flat; Red Hill), Stannum, Gough Co., New South Wales, Australia
1.6km (1.0 miles) Stannum Vale deep lead (Nine Mile deep lead; Wellington Vale lead; Red Hill lead), Stannum, Gough Co., New South Wales, Australia
References
Reference Search (possible matching items)
Report (issue)
N. CRAMSIE, DIRECTOR GEOLOGICAL SURVEY OF NEW SOUTH WALES i Original typing: Review: Cartography: Cover...from the coast south of Evans Head (see Photograph 12). Insets are: cut blue and gold New England sapphires...(lower left, see Photograph 34); and crystals of cassiterite (dark brown) in a quartz–topaz vein, Taronga...Survey of New South Wales, Sydney, xii + 292 pp, with CD-ROM. Edited by: R.A. Facer © New South Wales Department...northeastern New South Wales and extends over a significantly mineralised portion of the southern New England
 
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