Marble is a non-foliated metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite.
Geologists use the term "marble" to refer to metamorphosed limestone; however stonemasons use the term more broadly to encompass unmetamorphosed limestone.
Marble is commonly used for sculpture and as a building material.
The word "marble" derives from the Greek "μάρμαρον" (mármaron), from "μάρμαρος" (mármaros), "crystalline...
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Marble is a non-foliated metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite.
Geologists use the term "marble" to refer to metamorphosed limestone; however stonemasons use the term more broadly to encompass unmetamorphosed limestone.
Marble is commonly used for sculpture and as a building material.
The word "marble" derives from the Greek "μάρμαρον" (mármaron), from "μάρμαρος" (mármaros), "crystalline rock", "shining stone", perhaps from the verb "μαρμαίρω" (marmaírō), "to flash, sparkle, gleam". This stem is also the basis for the English word marmoreal, meaning "marble-like."
Whilst the English term resembles the French marbre, most other European languages (e.g. Spanish mármol, Italian marmo, Portuguese mármore, German, Norwegian, Danish and Swedish marmor, Armenian marmar, Dutch marmer, Polish marmur, Turkish mermer, Czech mramor and Russian мрáмор ) follow the original Greek.
Marble is a rock resulting from metamorphism of sedimentary...
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