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Natural Science in Archaeology

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136 6 Soft Stones and Other Carvable Materials<br />

called any red argillites catl<strong>in</strong>ite. However, the name should be reserved for rock of a<br />

specific m<strong>in</strong>eral composition. Other argillites and related rocks that were used for pipes<br />

should be called pipestone. Sigstad (1970) has developed a field test for catl<strong>in</strong>ite.<br />

Although the best-known catl<strong>in</strong>ite quarry is <strong>in</strong> southwestern M<strong>in</strong>nesota, there are<br />

similar deposits <strong>in</strong> Wiscons<strong>in</strong>, Ohio, Arizona, South Dakota, and Kansas (Berg 1938;<br />

Gunderson 1982). The trade <strong>in</strong> catl<strong>in</strong>ite extended from the Atlantic to the Pacific and<br />

north <strong>in</strong>to Canada. Pipes found <strong>in</strong> Hopewellian mounds <strong>in</strong> Erie County, Ohio, have<br />

been sourced to Wiscons<strong>in</strong> pipestone (Fredrickson 1981). Catl<strong>in</strong>ite pipes, beads,<br />

and ornaments were found among the historic Iroquois of New York (Wray 1957).<br />

Pipes and other objects carved of this stone have been found throughout the Northern<br />

Great Pla<strong>in</strong>s (Morey 1983). The M<strong>in</strong>nesota Geological Survey worked at the<br />

Pipestone National Monument dur<strong>in</strong>g 1980–1981. Their work resulted <strong>in</strong> the identification<br />

of three sites <strong>in</strong> the southern m<strong>in</strong>e area and five sites <strong>in</strong> the northern m<strong>in</strong>e<br />

area that have the highest potential for easily obta<strong>in</strong>able resources with m<strong>in</strong>imum<br />

extraction effort (Morey 1983).<br />

6.7 Other Carved Stone<br />

Porphyry. Porphyry from Mons Porphyrites quarries <strong>in</strong> the Red Sea mounta<strong>in</strong>s<br />

(present day Gebel Dukhan) was one of the most valued stones used for build<strong>in</strong>g<br />

decoration and for sculpture throughout the Roman Empire. Also called “imperial<br />

porphyry” by Pl<strong>in</strong>y, this red-to-purple porphyry was used for columns, baths,<br />

vases, and boxes (N.H. 36.57, 88). Delbrueck (1932) has produced an extensive<br />

monograph on the use of porphyry <strong>in</strong> the ancient world. His chapter on the written<br />

sources by author, <strong>in</strong>scriptions, ostraka, and papyri is of particular importance. The<br />

Egyptians employed porphyry to carve sph<strong>in</strong>xes and statues. In 1994, a previously<br />

unknown black porphyry quarry was discovered nearby (Peacock and Maxfield<br />

1995). The Romans imported green porphyry from Sparta, rosso antico from Cape<br />

Taenarum, and breccia from a region that extended from northwest Turkey to Rome.<br />

Other porphyry came from Chalcis and Scyros. Dur<strong>in</strong>g the Middle Ages, porphyry<br />

was used throughout Europe for statuary, columns, altar pieces, furniture or parts of<br />

furniture, and as a f<strong>in</strong>ish<strong>in</strong>g stone. In Sicily, this material was particularly favored<br />

by dynastic rulers to fashion their tombs. In Istanbul (ancient Constant<strong>in</strong>ople), porphyry<br />

sarcophagi are found <strong>in</strong> the Church of the Holy Apostles, the burial site of<br />

many Eastern emperors (Deér 1959).<br />

Mica. Muscovite mica is a sheet silicate m<strong>in</strong>eral with perfect two-dimensional<br />

cleavage. It is colorless and transparent <strong>in</strong> th<strong>in</strong> sheets. It has a vitreous to pearly luster.<br />

Muscovite is common rock-form<strong>in</strong>g m<strong>in</strong>eral and form large sheets [more than a<br />

meter across] <strong>in</strong> granite pegmatites. Its low hardness [2–2.5] makes it very easy to<br />

carve (Fig. 6.8). The term for mica throughout Ch<strong>in</strong>ese history was cloud mother.<br />

A treatise <strong>in</strong> 1070 states, “Mica grows between earth and rocks. It is like plates <strong>in</strong><br />

layers which can be separated, bright and smooth. The separate lam<strong>in</strong>ae look like<br />

the w<strong>in</strong>gs of a cicada.”

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