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- Dimensions height: 15 cm, length: 11 cm, width: 6.7 cm
- ID no. ZNG PAN B-V-17/142.1
- Museum The Geological Museum of the Institute of Geological Sciences, Polish Academy of Sciences
- Subjects nature, excavated from the earth
- Material mineral
- Object copyright The Geological Museum of the Institute of Geological Sciences, Polish Academy of Sciences
- Digital images copyright public domain
- Digitalisation RDW MIC, Małopolska's Virtual Museums Plus project
- Tags mineral , crystal , nature , 3D plus , WMM Plus , public domain
Calcite is a mineral of the carbonate class, also known as calcium carbonate. Its name derives from the Greek word chalix and the Latin word calx (calcis) – meaning “calcium”, which is a reference to the traditional application of this mineral. It develops isometric, plate, prism and needle crystals.
more Calcite is a mineral of the carbonate class, also known as calcium carbonate. Its name derives from the Greek word chalix and the Latin word calx (calcis) – meaning “calcium”, which is a reference to the traditional application of this mineral. It develops isometric, plate, prism and needle crystals. It often develops twin forms and multiple compounds. It takes the form of rhombohedrons (each side of such a solid is a rhomb) and sharply ended scalenohedrons (polyhedrons resembling a double pyramid in shape). It is distinguished by the richness of its forms – at present, more than two thousand forms of its crystals and combinations are known.
Calcite is a common rock-forming mineral of sedimentary rocks (limestones, marls, calcium sandstones, and others). It often occurs in ore veins, among melaphyres and basalts, forming speleothes in empty spaces, in caves. It is a component of skeletons of many organisms.
Elaborated by Barbara Kietlińska-Michalik (The Geological Museum of the Institute of Geological Sciences, Polish Academy of Science), editorial team of Małopolska’s Virtual Museums, © all rights reserved
Bibliography:
Jerzy Żaba, Ilustrowana Encyklopedia Skał i Minerałów, Katowice 2010.
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