PERSONAL DETAILS: MAIN PAGE: SPOT PRICES: DEPOSIT MODELS: IDENTIFYING MINERALS: CARBONATES: HALIDES NATIVE ELEMENTS: OXIDES: SILICATES: SULPHATES: SULPHIDES: LINKS: SIGN GUESTBOOK: View Guestbook: View Old Guestbook: |
adamantine lustre. Acicular (needle shaped) crystals are common but malachite usually forms as either a film on other copper minerals or as botryoidal/reniform masses with a banded structure. Hardness is between 3.5-4 with a perfect cleavge. Malachite forms in the oxidation zones of copper deposits as a result of the reaction of sulphides with carbonates. It is associated with azurite, cuprite and native copper. World class deposits in Russia (Urals), Zaire (Katanga), Zambia, Arizona (Bisbee) and Germany (Betzdorf).
to adamantine with a hardness of 3.5-4. Crystals are either elongate or tabular-prismatic in habit but can also form complex radiating aggregates. Azurite is a common secondary mineral in the oxidised zone of copper deposits along with malchite. It forms at lower temperatures than malachite and can often be replaced by it through hydration. Azurite is also associated with carbonate rocks. World class deposits are rare as it is less widely distributed than malachite. Some good crystals are found in Arizona (Bisbee), France (Lyon), Greece (Laurium) and Namibia (Tsumeb).
pearly lustre. Crystals are rhombohedral with curved, striated faces. Botryoidal, compact and oolitic masses are common. Hardness is between 3.5-4.5 with a perfect rhombohedral cleavage. Siderite is common in low to medium temperature hydrothermal veins associated with fluorite, barite, galena and sphalerite. Even more common in sedimentary deposits as concretions in clays and shales. World class deposits found in Austria (Styria), England (Cornwall), Brazil, Canada and Greenland.
|