Flint (or flintstone) is a har, sedimentary cryptocrystalline form of the mineral quartz, categorized as a variety of chert. Flint is usually dark grey, black, green, white, or deep brown in colour, and often has a waxy appearance. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones. From a petrological point of view, "flint" refers specifically to the form of chert which occurs in chalk or marly limestone. Similarly, "common chert" (sometimes referred to simply as "chert") occurs in limestone.