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The granite of the dimension-stone industry along with truly granitic rock also includes gneiss, gabbro, anorthosite and even some sedimentary rocks. Natural stone is used as architectural stone (construction, flooring, cladding, counter tops, curbing, etc.) and as raw block and monument stone for the funerary trade.
A stoup from brown Slivenec marble in the church in Dobřichovice [4] Český Šternberk marble (šternberský mramor) from Český Šternberk, Benešov District: white; Pernštejn marble (pernštejnský mramor) from Nedvědice, Brno-Country District: white; Nehodiv marble (nehodivský mramor) from Nehodiv, Klatovy District: grey
Verd antique is used like marble especially in interior decoration and occasionally as outdoor trim, although the masses are frequently jointed and often only small slabs can be secured. The ancient Romans quarried it especially at Casambala, near Larissa, Thessaly, in Greece. [8] This variety was known as marmor thessalicum or
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Carrara marble, or Luna marble (marmor lunense) to the Romans, is a type of white or blue-grey marble popular for use in sculpture and building decor. It has been quarried since Roman times in the mountains just outside the city of Carrara in the province of Massa and Carrara in the Lunigiana , the northernmost tip of modern-day Tuscany , Italy.
The most common slab format is 3040 mm x 1440 mm for Quartz and 3050 mm x 1240 mm for Breton-based marbles, but other sizes like 3040 mm x 1650 mm are produced according to market demand. Engineered stone is non porous, [ 7 ] more flexible, and harder than many types of natural stone.
Sylacauga marble, also commonly known as Alabama marble, is a marble that is found in a belt running through Talladega County, Alabama. [1] It is prized for its pure white color and its crystalline structure. The stone is named after the town of Sylacauga, Alabama, which is sometimes called "the Marble City". [2]
The marble's creation is owed to high level metamorphic processes in a contact zone with dome-like bulges of migmatite. [1] The two types of stone alternate in layers and the marble has a thickness of up to 30 metres in old fissures. The layers strike in a northeasterly direction. Naxian marble is over 98% calcite.
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