Garnet vs. Quartz

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Garnetnoun

(mineral) A hard transparent mineral that is often used as gemstones and abrasives.

Garnetnoun

A dark red color, like that of the gemstone.

Garnetadjective

Of a dark red colour.

Garnetnoun

A mineral having many varieties differing in color and in their constituents, but with the same crystallization (isometric), and conforming to the same general chemical formula. The commonest color is red, the luster is vitreous, and the hardness greater than that of quartz. The dodecahedron and trapezohedron are the common forms.

Garnetnoun

A tackle for hoisting cargo in or out.

Garnetnoun

any of a group of hard glassy minerals (silicates of various metals) used as gemstones and as an abrasive

Garnet

Garnets ( ) are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives. All species of garnets possess similar physical properties and crystal forms, but differ in chemical composition.

Quartznoun

(mineral) The most abundant mineral on the earth's surface, of chemical composition silicon dioxide, SiO2. It occurs in a variety of forms, both crystalline and amorphous. Found in every environment.

Quartznoun

A form of silica, or silicon dioxide (SiO2), occurring in hexagonal crystals, which are commonly colorless and transparent, but sometimes also yellow, brown, purple, green, and of other colors; also in cryptocrystalline massive forms varying in color and degree of transparency, being sometimes opaque.

Quartznoun

colorless glass made of almost pure silica

Quartznoun

a hard glossy mineral consisting of silicon dioxide in crystal form; present in most rocks (especially sandstone and granite); yellow sand is quartz with iron oxide impurities

Quartz

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2.

Garnet Illustrations

Quartz Illustrations

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