Marble Stone is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite rock. Metamorphism causes variable recrystallization of the original carbonate mineral grains.

The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the original carbonate rock (protolith) have typically been modified or destroyed.

*Colour may vary from that shown


KCMS 1002
KCMS 1002
KCMS 1102
KCMS 1102
KCMS 1104
KCMS 1104
KCMS 1106
KCMS 1106
KCMS 1208
KCMS 1208
KCMS 1211
KCMS 1211
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