Sard is a reddish-brown
chalcedony, SiO
2, much used by the ancients as a
gemstone.
Pliny the Elder states that it was named from
Sardis, in
Lydia, where it was first discovered; but the name probably came with the stone from
Persia (Pers. sered, yellowish-red). Sard was used for
Assyrian cylinder-seals,
Egyptian and
Phoenician scarabs, and early
Greek and Etruscan gems. The
Hebrew odem (translated sardius), the first stone in the High Priest's breastplate, was a red stone, probably sard but perhaps
carnelian or red
jasper. Some kinds of sard closely resemble carnelian, but are usually rather harder and tougher, with a duller and more hackly fracture.
Mineralogically the two stones pass into each other, and indeed they have often been regarded as identical, both being chalcedonic
silica colored with
iron oxide. The range of colors in sard is very great, some stones being orange-red, or hyacinthine, and others even golden, while some present so dark a brown color as to appear almost black by reflected light. The hyacinthine sard, resembling certain
garnets, was the most valued variety among the ancients for cameos and intaglios. Dark-brown sard is sometimes called sardoine, or sardine, while certain sards of yellowish color were at one time known to collectors of engraved gems as
beryl.
References
- http://www.mindat.org/min-7607.html