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A OPEN PIT MINING AÇIK OCAK MADENCİLİĞİ

A OPEN PIT MINING AÇIK OCAK MADENCİLİĞİ

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M. Coli, M. Baldi<br />

Figure 5. General view of the main Roman<br />

sledge-way driven above the ancient quarries<br />

of the bekhen-stone opened at the base of the<br />

slope.<br />

Then, the collected blocks were dressed in<br />

situ to the right size, because the layering<br />

represents a natural surface of weakness, the<br />

hand worked blocks could break during the<br />

dressing.<br />

The hand worked blocks were not finished<br />

or polished, usually these actions were<br />

completed only at the final destination, so<br />

that the finished surfaces were not damaged<br />

during the transport.<br />

4.1.3 Use<br />

The bekhen-stone is a beautiful grey/green<br />

ornamental stone prized for all kinds of<br />

artistic production. It was already quarried in<br />

the Predynastic period (Nagada I e Nagada II<br />

- Lazzarini 2002), and a large number of<br />

artifacts in bekhen-stone have been found in<br />

pyramids, tombs and temples, many ancient<br />

Pharaohs having had their sarcophagus made<br />

with bekhen-stone (e.g.: Unas, Teti, Pepy I,<br />

Merenre - Old Kingdom) (Aston et al.,<br />

2000). The statue of Darius in Persepolis<br />

was made of bekhen-stone, and the Romans<br />

largely used the bekhen-stone both for<br />

mediatic purpose and for the production of<br />

bowls, statues and sarcophaguses, until the<br />

III Century A.D. (Borghini, 1989; Lazzarini,<br />

2002; Giampaolo et al., 2008).<br />

The quarries were still being worked<br />

during the late Roman times, but with the<br />

decline of the Empire the request for bekhenstone<br />

diminished: many blocks still lie<br />

abandoned along the wadi.<br />

4.2 Breccia Verde Antica<br />

Breccia Verde Antica (breccia verde<br />

d’Egitto) was for the Romans Lapis<br />

hecatontalithos but also Lapis<br />

hexacontalithos (Lazzarini, 2002)<br />

(http://www.museo.isprambiente.it/schedeM<br />

appa.page?docId=381).<br />

We numbered two quarries of “Breccia<br />

Verde Antica”.<br />

4.2.1 - Geology<br />

Breccia Verde Antica was quarried from the<br />

Um Had Conglomerate Member of the<br />

Hammamat Group, it is a dark-, purplishand<br />

greenish-grey to mainly greyish-green,<br />

chloritic siltstone, with a few layers of<br />

pudding (Harrel et al., 2002). This last is a<br />

clast-supported pudding with greenish<br />

chloritic matrix (locally reddish), siltgrained,<br />

with a few levels of well-rounded<br />

sub-spherical pebbly to cobbly (until 25cm<br />

in diameter) clasts of many different<br />

lithologies (granites, limestones, metabasites,<br />

chert, …) and colours (white, pink,<br />

red, yellow, brown, green and grey).<br />

The pudding layers have a bimodal<br />

texture, with the pebbles surrounded and<br />

supported by a coarse- to very coarsegrained<br />

sandy matrix with chlorite, sericite<br />

and epidote plus minor amounts of calcite<br />

and iron oxides. The two main pudding<br />

layers are up to a meter thick, and both were<br />

quarried as “Breccia Verde Antica”.<br />

The lithological layering dips of about 45°<br />

towards East and represents a natural<br />

discontinuity.<br />

The pudding layers are cut by two joint<br />

sets which lie at about 90° to each other, and<br />

trend around E-W and N-S respectively,<br />

lying normally to the layering.<br />

Discontinuities are spaced a few meters apart<br />

and delimit natural blocks some cubic meters<br />

in volume.<br />

4.2.2 - Quarrying<br />

Quarriers used the natural discontinuities as<br />

preferential surfaces to force the block to fall<br />

down, therefore the two quarries were<br />

opened on the northern wadi side where the<br />

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