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Marble mis-nomers: Cetechovice marble (cetechovický mramor) from Cetechovice, Kroměříž District: coloured [c] Karlík marble (karlický mramor), from Barrandien, Karlík, Prague-West District: black with gold-yellow-colour veins [d] Podol marble (Podolský mramor), from Vápenný Podol, Chrudim District: white, grey-white, rosy [e]
Marquetry (also spelled as marqueterie; from the French marqueter, to variegate) is the art and craft of applying pieces of veneer to a structure to form decorative patterns or designs. The technique may be applied to case furniture or even seat furniture, to decorative small objects with smooth, veneerable surfaces or to freestanding pictorial ...
Cultured marble countertops are man made vanity tops that have the appearance of and resemble real stone marble. [6] [unreliable source?] Cultured marble countertops are made by mixing high strength polyester resin and real marble stone dust. The combination is then formulated with additional chemicals and poured into a cast mold.
Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite. Metamorphism causes variable re-crystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.
Tuckahoe marble (also known as Inwood and Westchester marble) is a type of marble found in southern New York and western Connecticut in the Northeastern United States. Part of the Inwood Formation of the Manhattan Prong , it dates from the Late Cambrian to the Early Ordovician ages (~484 ma ago ).
Tufa columns at Mono Lake, California. Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertine or thermogene travertine.
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