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Marble from Fauske Municipality in Norway Blocks of Carrara marble in Italy. The following is a list of various types of marble according to location. (NB: Marble-like stone which is not true marble according to geologists is included, but is indicated by italics with geologic classification given as footnote.
Bayburt (Armenian: Բայբերդ, romanized: Bayberd) [2] is a city in northeast Turkey lying on the Çoruh River.It is the seat of Bayburt Province and Bayburt District. [3]
Marble is a metamorphic rock derived from limestone, composed mostly of calcite (a crystalline form of calcium carbonate, CaCO 3).The original source of the parent limestone is the seabed deposition of calcium carbonate in the form of microscopic animal skeletons or similar materials.
Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO 3) or dolomite (CaMg(CO 3) 2) that have recrystallized under the influence ...
Parian marble is a fine-grained, semi translucent, and pure-white marble quarried during the classical era on the Greek island of Paros in the Aegean Sea. A subtype, referred to as Parian lychnites , was particularly notable in antiquity by ancient Greeks as a material for making sculptures .
The whiteness of the marble, its homogeneous form, and the micro-granular structure generate a high demand for Sivec marble on the international market. [ citation needed ] Sivec®, or Bianco Sivec, is the registered name for this fine-grained white dolomitic marble.
Grand Antique marble (also Celtic marble (Latin: marmor celticum), Grand Antique of Aubert, and known in Roman times as Marmor Aquitanicum), is a prestigious marble, composed of clasts of black limestone and white calcite, quarried near Aubert-Moulis in France.
The Cockeysville Marble is a Precambrian, Cambrian, or Ordovician marble formation in Baltimore, Carroll, Harford and Howard Counties, Maryland. It is described as a predominantly metadolomite , calc- schist , and calcite marble , with calc- gneiss and calc- silicate marble being widespread but minor.
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