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Natural Science in Archaeology

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52 3 Exploitation of M<strong>in</strong>eral and Rock Raw Materials<br />

Fig. 3.1 Granite gr<strong>in</strong>der,<br />

M<strong>in</strong>e Dunquash, Egyptian<br />

Eastern Desert<br />

Granites were used as build<strong>in</strong>g or monumental stone <strong>in</strong> nearly every country<br />

where good outcrops occurred. Granite columns are quite common <strong>in</strong> build<strong>in</strong>gs<br />

of Roman Spa<strong>in</strong>. Although many local granites were quarried for build<strong>in</strong>gs, many<br />

granite build<strong>in</strong>g stones were imported from a number of other Mediterranean<br />

region sources. Williams-Thorpe and Potts (2002) studied 152 granite columns<br />

from Spa<strong>in</strong> to determ<strong>in</strong>e their geologic provenance. Twenty-five columns were<br />

attributed to sources <strong>in</strong> western Turkey and the Italian Islands Elba/Giglio and<br />

Sard<strong>in</strong>ia.<br />

The granites of Aberdeen are the most famous of all build<strong>in</strong>g stones of Scotland.<br />

The Shap granite of Cumbria, England, with p<strong>in</strong>k and white feldspar phenocrysts,<br />

was sought after as f<strong>in</strong>ish<strong>in</strong>g stone. F<strong>in</strong>land is well known for the rapakivi granite–<br />

a hornblende-biotite granite that has a texture <strong>in</strong> which large crystals of potassium<br />

feldspar are rimmed by a sodic plagioclase feldspar <strong>in</strong> a f<strong>in</strong>er-gra<strong>in</strong>ed matrix.<br />

Rapakivi is F<strong>in</strong>nish for “crumbly rock”, a name given to this rock because when<br />

exposed to the atmosphere it crumbles <strong>in</strong>to smaller pieces. Rapakivi granite is the<br />

material used <strong>in</strong> the stone churches <strong>in</strong> the Middle Ages <strong>in</strong> Åland <strong>in</strong> the Gulf of<br />

Bothnia between Sweden and F<strong>in</strong>land.<br />

In India, granites were commonly used for the lower stories of H<strong>in</strong>du temples<br />

and <strong>in</strong> cave temples. In Neolithic South India granites formed a significant percentage<br />

of querns and gr<strong>in</strong>dstones (Brumm et al. 2007).<br />

In South America the famous Inca high mounta<strong>in</strong> fortress at Machu Pichu was<br />

constructed largely of granite. In Italy the “Granito del foro” of architectural historians<br />

is a dist<strong>in</strong>ctive granodiorite (see Table 3.1) used <strong>in</strong> important monuments<br />

<strong>in</strong> ancient Rome. It was quarried from the famous Mons Claudianus deposits <strong>in</strong><br />

the Egyptian Eastern Desert (Peacock et al. 1994). Many other granodiorites and

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