quartz
Quartz is composed mainly by SiO2, and its structure is crystalline.

Quartz occurs in many varieties. Rock crystal is colourless quartz and sub-varieties include ghost quartz in which growth stages are marked by inclusions, and rutilated quartz (sagenite), which contains hair-like rods of rutile. Amethyst is purple; milk quartz is white; rose quartz is rose-red or pink, and is usually found massive rather than as crystals. Citrine is yellow and transparent and resembles topaz. Smoky quartz (sometimes called cairngorm) is smoky brown to nearly black. Some quartzes contain impurities that not only impart a colour but render them opaque. Ferruginous quartz is an example of this and is commonly brick-red or yellow.​

Distinguishing features: Crystal form, conchoidal fracture, vitreous lustre, hardness.

Occurrence: Quartz is one of the most widely distributed minerals. (Hamilton et al 1976, 128)

quartzflakes
quartz flakes