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Natural Science in Archaeology

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96 5 Gemstones, Seal Stones, and Ceremonial Stones<br />

Citr<strong>in</strong>e. Citr<strong>in</strong>e’s color varies from pale yellow, yellow, to yellow-brown or<br />

reddish-brown. Schmetzer (1988) has shown that color centers <strong>in</strong> citr<strong>in</strong>e can be<br />

bleached with heat<strong>in</strong>g. It is transparent to translucent. The name orig<strong>in</strong>ates from the<br />

French citron (lemon). It is often erroneously called “topaz.” It was used as gems<br />

and seal stones. Citr<strong>in</strong>e is much rarer <strong>in</strong> nature than amethyst. Amethyst but not<br />

citr<strong>in</strong>e is noted <strong>in</strong> the Bible [as one of the gemstones used <strong>in</strong> decorat<strong>in</strong>g the high<br />

priest’s breastplate].<br />

In ancient times citr<strong>in</strong>e was carried as a protection aga<strong>in</strong>st snake venom. It was<br />

sometimes called “sunstone” because, as a result of its color, it was though capable<br />

of hold<strong>in</strong>g sunlight. <strong>Natural</strong> citr<strong>in</strong>es are rare so today citr<strong>in</strong>es are often heat treated<br />

amethyst or smoky quartz. Citr<strong>in</strong>e can change color permanently if left <strong>in</strong> direct<br />

sunlight. It was first used <strong>in</strong> jewelry <strong>in</strong> Greece <strong>in</strong> the Hellenistic Period, from the 4th<br />

through the first century BCE. The first use by the Romans was <strong>in</strong> <strong>in</strong>taglios (a gem<br />

carved <strong>in</strong> negative relief) and cabochons <strong>in</strong> the first centuries CE.<br />

Smoky Quartz. Smoky quartz varies from pale smoky-brown to almost black<br />

and from transparent to nearly opaque. It is also called cairngorm (after a locality<br />

<strong>in</strong> Scotland) or morion from Lat<strong>in</strong> mormorion. This may be the m<strong>in</strong>eral Pl<strong>in</strong>y calls<br />

chrysolithus, which by his account came from India (N.H. 37.90, 91, 101, 126,<br />

127). Another possibility is that smoky quartz is the m<strong>in</strong>eral Pl<strong>in</strong>y calls capnias.<br />

He does not list its source (N.H. 37.118, 128). It was used as a gemstone and seal<br />

stone. Smoky quartz crystals were used to decorate the breastplate of the high priest<br />

<strong>in</strong> Old Testament times.<br />

Rose Quartz. This gemstone’s name refers to its color, which varies from pale<br />

p<strong>in</strong>k to deep rose red, occasionally with a purplish t<strong>in</strong>ge. It sometimes exhibits<br />

dist<strong>in</strong>ct asterism. Maschmeyer and Lehmann (1983) have identified color centers <strong>in</strong><br />

rose quartz. This could be the m<strong>in</strong>eral Pl<strong>in</strong>y calls anteros (N.H. 37.123). It was used<br />

as a gemstone and seal stone.<br />

Tiger-Eye/Cat’s Eye. This m<strong>in</strong>eral can be found <strong>in</strong> many colors from yellow,<br />

yellow-brown, brown, reddish-brown, through bluish, grayish-green, or green, and<br />

it was used for both gems and seal stones.<br />

Aventur<strong>in</strong>e normally conta<strong>in</strong>s small <strong>in</strong>clusions. This material has also been<br />

called sandastros. Accord<strong>in</strong>g to Pl<strong>in</strong>y, sandastros came from India and southern<br />

Arabia (N.H. 37.100–102). He also mentions a variety called sandrisites but does<br />

not list its source (N.H. 37.10). It was used for gems and seal stones.<br />

5.2.2 Cryptocrystall<strong>in</strong>e Varieties<br />

Chalcedony can be white, grayish, blue, brown, or black. It has a waxy luster and<br />

is transparent to translucent. The name is derived from Chalcedon, an ancient city<br />

of Bithynia <strong>in</strong> Asia M<strong>in</strong>or. Ancient sources of this m<strong>in</strong>eral were located <strong>in</strong> what<br />

is now India, Yemen, and Iraq. It also occurs <strong>in</strong> Egypt’s Eastern Desert, Western<br />

Desert, S<strong>in</strong>ai, and other locations. It was used there as early as Predynastic times<br />

(Lucas 1989:392). Pl<strong>in</strong>y’s capnias may be chalcedony. He does not list its source

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