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Natural Science in Archaeology

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5.5 Oxide M<strong>in</strong>erals 113<br />

Freshwater pearls were collected by Native Americans. They have been found <strong>in</strong><br />

the ancient burial mounds of the Hopewell people <strong>in</strong> Ohio. Conversely, aborig<strong>in</strong>al<br />

peoples of Australia regard pearls as a nuisance s<strong>in</strong>ce they occasionally cracked<br />

their teeth on them while d<strong>in</strong><strong>in</strong>g on north coast oysters (Ward 1985). Freshwater<br />

pearls have also been found <strong>in</strong> rivers <strong>in</strong> the British Isles and cont<strong>in</strong>ental Europe.<br />

Although the technique for grow<strong>in</strong>g cultured pearls was not developed by the<br />

Japanese until the early twentieth century, the Ch<strong>in</strong>ese developed a method for mak<strong>in</strong>g<br />

“pearl” Buddhas as early as the twelfth century. A t<strong>in</strong>y carv<strong>in</strong>g or metal cast<strong>in</strong>g<br />

of a Buddha was cemented to the <strong>in</strong>side of a freshwater mussel until it was coated<br />

with nacre (Ward 1985). These were used as amulets and decorations.<br />

Azurite, Cu 3 (CO 3 ) 2 (OH) 2 , has a hardness from 3.5 to 4 and a density of 3.77. It<br />

is found <strong>in</strong> shades of light to dark blue. Pl<strong>in</strong>y states that cyanus (azurite crystals)<br />

came from Scythia, Cyprus, and Egypt. Lapis Armenius came from Armenia and<br />

Spa<strong>in</strong> (N.H. 35.47).<br />

Malachite, Cu 2 CO 3 (OH) 2 , has a hardness between 3.5 to 4 and a density of 4.05. It<br />

is bright green to dark or blackish-green <strong>in</strong> color. Its name is derived from the Greek<br />

mallow (green). In the New World, the deposits exploited between 200–800 CE<br />

near Chalchihuites, Mexico, <strong>in</strong>cluded malachite (Weigand 1994). Malachite was<br />

used <strong>in</strong> the Old World at least as early as the fifth millennium BCE. Malachite<br />

occurs <strong>in</strong> S<strong>in</strong>ai, Egypt. It was rarely used for jewelry by the Egyptians, although a<br />

few Predynastic beads and several later ornaments are known (Lucas 1989). Pl<strong>in</strong>y<br />

does not list a source for molochitis (N.H. 37.114). He mentions a number of other<br />

materials that could have been malachite. Pl<strong>in</strong>y identifies chrysocolla as com<strong>in</strong>g<br />

from Cyprus, Armenia, Macedonia, and Spa<strong>in</strong> (N.H. 33.4, 86–93, 161; 35.30, 47,<br />

48). He also mentions chalcosmaragdus from Cyprus (37.74). Cosmetics and pa<strong>in</strong>t<br />

pigment were made from malachite, and it was carved <strong>in</strong>to beads, gems, and decorative<br />

objects.<br />

Gypsum, CaSO 4 ·2H 2 O, has a hardness of 2 and a density of 2.32. The name<br />

comes from the Greek word for plaster. Alabaster is a compact, f<strong>in</strong>e-gra<strong>in</strong>ed variety<br />

of gypsum. It is found <strong>in</strong> white, cream, or variegated colors. Its ancient name<br />

was orig<strong>in</strong>ally given to several materials from which o<strong>in</strong>tment vases called “alabastra”<br />

were made (from alabastron), but its name may ultimately derive from a<br />

town <strong>in</strong> Egypt. Alabaster occurs abundantly <strong>in</strong> the Eastern Desert of Egypt and at<br />

El-Amarna. Jewelry and furniture <strong>in</strong>laid with alabaster were found <strong>in</strong> the tomb of<br />

Tutankhamen. Beads are known from the 18th Dynasty and later (Lucas 1989).<br />

Cyl<strong>in</strong>der seals, carv<strong>in</strong>gs, statues, and small decorative objects were carved from<br />

alabaster. It was also used for beads and jewelry <strong>in</strong>lay.<br />

5.5 Oxide M<strong>in</strong>erals<br />

Hematite, Fe 2 O 3 , varies <strong>in</strong> hardness from 5 to 6 and has a density of 5.26. It is<br />

steel gray to iron-black and sometimes appears rusty or iridescent; th<strong>in</strong> fragments<br />

can appear deep blood red. Massive and earthy material is dull brownish-red to

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