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・ Caledonian Road & Barnsbury railway station
・ Caledonian Road tube station
・ Caledonian Road, London
・ Caledonian Sleeper
・ Caledonian Stadium
・ Caledonian Stadium (South Africa)
・ Caledonian Steam Packet Company
・ Caledonian Thebans RFC
・ Caledonian Union
・ Caledonians
・ Caledonians (disambiguation)
・ Caledonians F.C.
・ Caledonica
・ Caledoniscincus
・ Caledoniscincus atropunctatus
Caledonite
・ Caledonomorpha
・ Caledonomorpha elegans
・ Caledophia
・ Caledothele
・ Caledothele elegans
・ Caledyschirius
・ Calefaction
・ Calefactory
・ Calefare
・ Calefax
・ Calega Panzan
・ Calegari
・ Caleidocrinus
・ Caleigh Peters


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Caledonite : ウィキペディア英語版
Caledonite

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.
==Collectible properties==

Caledonite'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.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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