Marble is a metamorphic rock formed when limestone recrystallises under high pressure and temperature. The original limestone fabric disappears and a dense interlocking network of calcite crystals takes its place. That explains its behaviour: marble is dense, takes a mirror polish, and shows the characteristic veining that comes from impurities in the parent rock.

Chemically, marble is almost entirely calcium carbonate. On the Mohs scale calcite sits at 3 — soft, roughly scratchable with a copper coin. Granite, with quartz at 7, is considerably harder.

Mohs hardness: marble versus graniteCalcite (marble)Calcite (marble): 3 Mohs3 MohsQuartz (in granite)Quartz (in granite): 7 Mohs7 Mohs
Mohs hardness of calcite (the mineral marble consists of) and of quartz in granite. A higher value means more scratch resistant.

Trade name versus geology

Be aware that the stone trade calls many materials “marble” that are geologically limestone or travertine. In practice this matters little, because they behave similarly, but in a specification or a conservation report the stone type has to be named precisely.

Properties and limitations

Working with it and looking after it

Related terms

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