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Natural Science in Archaeology

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11.2 Build<strong>in</strong>g Stone 251<br />

Fig. 11.2 The great rock-cut<br />

temple of Abu Simbel of<br />

Rameses II, south of Aswan<br />

on the west bank of the Nile,<br />

carved out of sandstone rock<br />

cliffs about 1280 BCE<br />

limestones and marbles, but they have relatively high compressive strength. The<br />

often severe directional weaknesses <strong>in</strong> metamorphic rocks frequently preclude their<br />

use <strong>in</strong> large-scale structures. Follow<strong>in</strong>g are summaries of the physical and chemical<br />

characteristics of the major build<strong>in</strong>g stones. Readers may want to review these rock<br />

types <strong>in</strong> Chap. 3.<br />

11.2.1 Granite/Diorite<br />

A typical granite is composed of 65% feldspar, 25% quartz, and 10% hornblende.<br />

The hardness of feldspar and hornblende ranges from 5.0 to 6.5, and the hardness of<br />

quartz is 7.0. Thus, granite is a hard rock. Most granites possess structural features<br />

that are important <strong>in</strong> the quarry<strong>in</strong>g of dimension stone and material for monuments<br />

or statuary. One of the most important features is part<strong>in</strong>g. Fortunately, one direction<br />

of part<strong>in</strong>g is nearly vertical, and the other direction is nearly horizontal <strong>in</strong> outcrop.<br />

The ancient Egyptians took advantage of this <strong>in</strong> quarry<strong>in</strong>g their huge granite<br />

obelisks (Fig. 11.3). Granites normally provide high strength <strong>in</strong> all directions. The<br />

major drawback of granites is their tendency to spall off <strong>in</strong> th<strong>in</strong> layers.<br />

High-quality granites that were widely used for build<strong>in</strong>g stone occur throughout<br />

most of the British Isles, <strong>in</strong> northwestern France, <strong>in</strong> much of Scand<strong>in</strong>avia, <strong>in</strong><br />

Italy, and <strong>in</strong> Russia. Iron Age peoples <strong>in</strong> England used granite blocks picked up<br />

from moors. Perhaps the most famous architectural granitic rock is the syenite outcropp<strong>in</strong>g<br />

between Aswan and the first cataract of the Nile River. This rock has<br />

been exploited s<strong>in</strong>ce the First Dynasty for tombs, temples, and sarcophagi. It was<br />

exported to other parts of the Mediterranean for obelisks and statues. Other wellknown<br />

granites are the gray granite from Aswan that was used for build<strong>in</strong>gs <strong>in</strong><br />

Egypt and exported, and the red granite porphyry quarried near the first cataract of<br />

the Nile that was used for sph<strong>in</strong>xes and statues <strong>in</strong> Egypt. The Romans shipped this<br />

stone to Italy and other prov<strong>in</strong>cial cities throughout the Roman Empire.

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