Chinkuashih Mine (Jinguashi)
25.1170° N, 121.8500° E · ± 1 km
Enargite from New Taipei City, Taiwan, with photos of specimens from this locality.
Minerals found here
On the same specimen
Enargite at Chinkuashih Mine (Jinguashi)
Enargite blades capped or replaced by luzonite on beds of lustrous pyrite are typical for this mine.

Photo: Robert M. Lavinsky · CC BY-SA 3.0 · Source

Photo: Robert M. Lavinsky · CC BY-SA 3.0 · Source

Photo: Robert M. Lavinsky · CC BY-SA 3.0 · Source

Photo: Robert M. Lavinsky · CC BY-SA 3.0 · Source

Photo: Robert M. Lavinsky · CC BY-SA 3.0 · Source
- Formula
- Cu₃AsS₄
- Morphology
- Blades and elongated prisms, partly with parallel growth; often overgrown by or altered to luzonite
- Typical size
- Crystals mostly about 1 cm; specimens up to about 8 cm
- Color / luster
- Black with excellent metallic luster
- Associated minerals
- Luzonitepyrite
- Surface features
- Strongly striated faces
- Availability
- No longer available
- History
- Historic Japanese-era gold-copper mine, now depleted
Geology of the locality
- Setting
- Gold-copper mine
- Region
- New Taipei City
- Country
- Taiwan
Coordinates are those of Jinguashi in Ruifang District (Wikipedia). The mines were run by Taiwan Kogyo during Japanese rule and are described as depleted. Specimen labels also name the Pen-Shan ore body of this mine.
Sources: SRC-649
Sources
- SRC-649 · Website
JinguashiWikipedia contributors · Wikipedia - SRC-642 · Book
Handbook of Mineralogy - EnargiteAnthony, J.W.; Bideaux, R.A.; Bladh, K.W.; Nichols, M.C. · 2005 · Mineral Data Publishing / Mineralogical Society of America - SRC-656 · Website
File:Enargite-Luzonite-Pyrite-120825.jpg; File:Enargite-227628.jpg; File:Enargite-Luzonite-163254.jpg (Wikimedia Commons)Robert M. Lavinsky · Wikimedia Commons
Draft data from the Provenite workbook. Check entries against the cited sources before relying on them. Photos are open-licence images from Wikimedia Commons; the author and licence are given with each photo.