Petrographically marbles are massive rather than thin layered and consist of a.
Marble grain type.
Commercially it includes all decorative calcium rich rocks that can be polished as well as certain serpentines verd antiques.
Can see interlocking calcite crystals with the naked eye.
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Marble is commonly used for sculpture and as a building material.
It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is.
Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
The chromatic uniformity of its base the type of grain and the thickness as well as drawing of its veins are characteristic and unique to each variety.
Grain size medium grained.
Colour variable pure marble is white but marble exists in a wide variety of colours all the way through to black.
Hardness hard although component mineral is soft calcite is 3 on moh s scale of hardness.
Marble granular limestone or dolomite i e rock composed of calcium magnesium carbonate that has been recrystallized under the influence of heat pressure and aqueous solutions.