Mons Porphyrites
In five seasons, between
1994-1998 the Departments of Archaeology at the Universities of Southampton and
Exeter surveyed and excavated at the quarry complex of Mons Porphrites. Mons
Porphrites was the source of purple Imperial Porphyry, much sought after in the
Roman and Byzantine worlds and which has continued to exercise symbolic
influence in western society. The quarries lie in the Gebel Dokhan, or 'smoky
mountain', itelf situated in the Red Sea mountains of eastern Egypt. The purple
Imperial Porphyry is found nowhere else in the world, except in these mountains
(together with other types of Porphyry) and the Romans went to extraordinary
lengths to acquire substantial amounts of it.
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Porphyry bath |
The Gebel Dokhan massif
consists of a number of peaks generally around 1200m high, ranging up to 1626m
above sea level. It is however only 40 km from the sea, separated by a plain of
low rolling hills. The rocks within the range are dominated by the Pre-Cambrian
'Dokhan volcanics'. The Imperial Porphyry, a quartz andeite ignimbrite
lithified to form a dense, hard rock wih a well-developed system of joints is
only found over a small area (c. 6km2). In 1994 a new quarry for black Porphyry
was discovered by the team and named after Nick Bradford who discovered it.
The logistics of
extracting the Porphyry are incredible. The Porphyry can only be extracted in
workable blocks from the tops of 4 mountains, and the quarries are named
Lycabettos, Rammius, Lepsius and North-west. The first three were named
originally by the Nineteenth century explorer Schweinfurth. The difficulty of
the terrain meant that the workers were accommodated in separate villages from
the quarries, generally reasonably close. The two main areas of settlement
below the quarries are a fort in the Wadi Abu Ma'amel and another on the
southern flank of the Gebel Dokhan, named Badia. The whole complex was linked
by a system of footpaths and slipways down which the Porphyry would be brought
to the Wadi bed.
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Cairned slipway and footpath |
The footpaths zig-zag up
the hills, often revetted over difficult areas and generally narrow. The
slipways in contrast have a smooth gradient and are wider but still survive
from the tops of the mountain to the wadi bed or loading villages. The path of
the slipways is often marked by cairns, circular structures made of dry stone
walling. The slipways are particularly impressive for both their extent and
completeness. On reaching the wadi bed the evidence continues in the form of a
cistern and animal lines at Umm sidri and then a great loading ramp 8km futher
on, where it is believed the the stone would be loaded on to carts for the
journey to the Nile, 150km away, going via Badia on a road again delineated by
cairns that are still visible today.
The environment is harsh
with no readily available water, except for a number of shady rock pools which
may preserve water for some time. The local vegetation is sparce although Wadi
Umm Sidri has a number of Zizyphus Spina-Christi trees which may
indicate the presence of ground water. Other water is conserved in underground
pockets in the wadi system, which at Badia is a few metres deep but over 15m
below the surface at Umm Sidri. Two wells were dug to supply the workers and a
supply chain was set up to bring water from the Nile. Modern rainfall is
infrequent and is usually in deluges between October and December. These
occurred three times during the length of the project and resulted in
considerable movement of the boulders on the wadi bed.
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Fort at Badia |
The problem of supplying
food is little different to that of water. There is no local source of food to
support the workforce which could in antiquity have amounted to several hundred
men and the wildlife of any size is rare in the present day environment. The
climate can reach temperatures of 114 degrees F (45.6 degrees C) in the summer.
Surveys of the pottery,
faunal remains, botanical evidence, epigraphic evidence, textiles and small
finds have all been undertaken and the first volume of the final report will be
published in 2001. The evidence shows that the complex was used throughout the
Roman period but that its focus changed through time, possibly commencing with
the North-west quarries. There is evidence of the people that lived, worked and
visited the sites included many military personnel but also women and children.
The epigraphic evidence gives insights into their private lives but also the
bureaucracy that surrounded an Imperial undertaking of this size.