A recrystallized limestone that formed when the limestone softened from heat and pressure
and recrystallized into marble where mineral change occurred. The main consistency is calcium
and dolomite. Ranges in many colors and is usually heavily veined and shows lots of grains.
Hardness rates from 2.5 to 5 on the MOH Scale.
Marble is what's known as a metamorphic rock. It was once limestone, but over time,
with the combination of heat and pressure caused the limestone to re-crystallize. During this
stage is often when foreign substances entered the stone creating a wide range of colors,
textures, and veining.