About Diamonds

Diamonds take shape deep within the Earth, approximately 100 miles below the surface, where extreme temperature and pressure conditions converge. The carbon atoms in diamonds are intricately bonded in a uniform arrangement, extending in all directions. In stark contrast, graphite, another mineral composed solely of carbon, features a distinct formation process and crystal structure. The stark contrast is evident in their physical properties; graphite is remarkably soft and suitable for writing, while diamond's exceptional hardness is such that only another diamond can leave a scratch upon it.