Quick answerMarble forms when limestone is buried deep within the Earth’s crust and exposed to intense heat and pressure. Over millions of years, the calcite crystals within the limestone recrystallise into a dense, interlocking structure, creating the stone we recognise as marble.
That geological history also explains something every marble owner eventually discovers: marble is beautiful because of its mineral structure, but that same structure makes it vulnerable to acids such as lemon juice, wine and vinegar.
Every marble benchtop started somewhere very different from a kitchen.
Long before it became a slab, it was limestone. Before that, much of its calcium carbonate came from shells, coral and marine organisms settling on ancient seabeds.
Then geology took over.