pseudomorphs

navigate by keyword : acicular azurite blocky blue botryoidal carbonate chemical copper crystal crystallizes crystals fibrous fluids geology green greenbanded hydrothermal hydroxide macro malachite masses mineral monoclinic opaque precipitation prisms pseudomorphs rare rock slender stalagmitic stone tabular teal texture yellow

Agate Royalty Free Stock Photo
Agate Royalty Free Stock Photo
Breathtaking Double Exposure Russian Limestone Formations Reveal Geological Transformation Through Chalcedony Royalty Free Stock Photo
Glendonite - rare uncommon minerals Royalty Free Stock Photo
Textures of a Piece of Green Malachite Royalty Free Stock Photo
A cross section of the agate stone. Royalty Free Stock Photo
A cross section of the agate stone. Royalty Free Stock Photo
Macro Texture of Malachite Stone
Macro Texture of Malachite Royalty Free Stock Photo
A cross-section of agate Royalty Free Stock Photo
A cross-section of agate Royalty Free Stock Photo
Agate Royalty Free Stock Photo
A cross-section of agate Royalty Free Stock Photo
A cross-section of agate Royalty Free Stock Photo
Agate Royalty Free Stock Photo
Malachite is a copper carbonate hydroxide mineral, with the formula Cu2CO3OH2. This opaque, green-banded mineral crystallizes in the monoclinic crystal system, and most often forms botryoidal, fibrous, or stalagmitic masses, in fractures and deep, underground spaces, where the water table and hydrothermal fluids provide the means for chemical precipitation. Individual crystals are rare, but occur as slender to acicular prisms. Pseudomorphs after more tabular or blocky azurite crystals also occur.[4]


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