Caledonite, whose name derives from Caledonia, the historical name of its place of discovery (Scotland), is a richly colored blue-green sulfate-carbonate mineral of lead and copper with an orthorhombic crystal structure. It is an uncommon mineral found in the oxidized zones of copper-lead deposits.
| Caledonite | |
|---|---|
.jpg) Caledonite (green) on cerussite | |
| General | |
| Category | Sulfate minerals |
| Formula (repeating unit) | Cu2Pb5(OH)6CO3(SO4)3 |
| IMA symbol | Cdo[1] |
| Strunz classification | 7.BC.50 |
| Crystal system | Orthorhombic |
| Crystal class | Pyramidal (mm2) (same H-M symbol) |
| Space group | Pmn21 |
| Unit cell | a = 20.089(7) Å, b = 7.146(3) Å, c = 6.56 Å; Z = 2 |
| Identification | |
| Color | Blue; green |
| Crystal habit | Typically striated prismatic or tabular crystals; radial aggregates |
| Cleavage | [001] perfect; [100] distinct |
| Fracture | Uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 2.5–3 |
| Luster | Vitreous |
| Streak | Green-white; blue-green |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 5.6–5.8 |
| Optical properties | Biaxial (−) |
| Refractive index | nα = 1.818(3) nβ = 1.866(3) nγ = 1.909(3) |
| Birefringence | δ = 0.091 |
| Pleochroism | Weak |
| 2V angle | Measured: 85° |
| References | [2][3][4][5] |
Collectible properties
editCaledonite's primary use is a collector's mineral. Although it contains copper and lead, it is a secondary mineral and is not prevalent enough in any known deposits to be used as an ore. Caledonite, when developed into full crystals, can have a deep blue-green color reminiscent of secondary copper minerals. Its high lustre, on the other hand, is more like secondary lead minerals. Localities in which caledonite occurs as well developed crystals are quite rare and include the Mammoth-St. Anthony Mine at Tiger, Arizona, a few mines in California, such as the Reward Mine. A few other mines in Arizona and Chile have been known to produce samples.
Associated minerals
editGiven that caledonite is found in oxidized copper/lead deposits, it is frequently found in association with other copper and lead minerals. Frequently associated minerals include: linarite, malachite, cerussite, brochantite, anglesite, leadhillite, and azurite.[3]
Notes for identification
editCaledonite's blue color is a useful indicator, but insufficient, especially since one of its associates, linarite, is a vivid blue as well. Useful tests for determining if a specimen is caledonite include its density, streak, and crystal habit.
References
edit- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ Mineralienatlas
- ^ a b "Handbook of Mineralogy" (PDF). Archived from the original (PDF) on 2016-03-03. Retrieved 2016-12-20.
- ^ MinDat Listing
- ^ Webmineral Listing