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  2. Carrara marble - Wikipedia

    en.wikipedia.org/wiki/Carrara_marble

    Carrara marble has been used since the time of Ancient Rome, when it was called marmor lunense, or "Luni marble". [2] [3]In the Middle Ages, most of the quarries were owned by the Marquis Malaspina who in turn rented them to families of Carrara masters who managed both the extraction and transport of the precious material.

  3. Quartz - Wikipedia

    en.wikipedia.org/wiki/Quartz

    Quartz is, therefore, classified structurally as a framework silicate mineral and compositionally as an oxide mineral. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. [10] Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation ...

  4. Cataclasite - Wikipedia

    en.wikipedia.org/wiki/Cataclasite

    Due to quartz being the main mineral in many rocks in the brittle regime of the crust, the brittle-ductile transition for quartz can be a good indication of where cataclasites would form before ductile deformation plays a role. [2] This normally refers to the uppermost 10–12 km of the continental crust. [2]

  5. David (Michelangelo) - Wikipedia

    en.wikipedia.org/wiki/David_(Michelangelo)

    David is a masterpiece of Italian Renaissance sculpture in marble [1] [2] created from 1501 to 1504 by Michelangelo.With a height of 5.17 metres (17 ft 0 in), the David was the first colossal marble statue made in the High Renaissance, and since classical antiquity, a precedent for the 16th century and beyond.

  6. Calcarenite - Wikipedia

    en.wikipedia.org/wiki/Calcarenite

    The Pietra di Bismantova in the northern Apennine (Emilia Romagna region, northern Italy) is an example of calcarenite formation.. Calcarenite is a type of limestone that is composed predominantly, more than 50 percent, of detrital (transported) sand-size (0.0625 to 2 mm in diameter), carbonate grains.

  7. Undulose extinction - Wikipedia

    en.wikipedia.org/wiki/Undulose_extinction

    Undulose extinction of quartz in Orthogneiss. Undulose extinction or undulatory extinction is a geological term referring to the type of extinction that occurs in certain minerals when examined in thin section under cross polarized light.

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