The geography and geology of south-eastern EgyptBall, John
Science
The geography and geology of south-eastern Egypt
Ball, John
Geology -- Egypt; Physical geography -- Egypt
------------------+-----------+------------+-----------
Station. |Latitude N.|Longitude E.| Altitude
| | |above Sea.
------------------+-----------+------------+-----------
| | | metres.
| | |
Edfu | 24° 58′ | 32° 54′ | 90
| | |
Kanais | 25° 0 ′ | 33° 19′ | 205
| | |
Gariat Abu Medrik| 24° 55′ | 33° 41′ | 295
| | |
Samut | 24° 49′ | 33° 54′ | 340
------------------+-----------+------------+-----------
The next station after Samut appears to have been the ruins near
Gebel Dweig. Further on, after passing over the watershed, is
another station with two cisterns in a semicircular enclosure. The
road continues past Gebel Abu Had to the Wadi Gemal, where there are
two more cisterns, this time in a triangular enclosure, and thence
up to the Wadi Nugrus and Wadi Sikait to the mines. The Edfu-Sikait
road may have joined the Quft-Berenice road at the Wadi Gemal station.
A third ancient road is believed to have led northward from Berenice
to Qoseir, along the coast; while a fourth, from near Dakka on the
Nile up the Wadi Alaqi to the gold mines of the south, is now a
regular route to the Nile Valley Company’s mine of Um Gariart.
The =ancient emerald mines of Zabara and Sikait= consist of numerous
irregular shafts, mostly of no very great depth, excavated in schists
of micaceous and talcose types. The =old gold mines=, such as those
at Sukari, Um Eleiga, Seiga, Romit, and the Darahib district, are on
a considerable scale, excavations having been carried on in quartz
veins to fair depths. The dwellings at the mines were for the most
part only miserable hovels of rubble stone. A view of those of Um
Eleiga is given on Plate IV. The ancient quartz-grinding mills, mostly
made of a hard diorite, are frequently found among the ruins of the
hovels. There is no clear evidence that any of the mines yielded a
very rich output; the workings were of the nature of penal settlements
(Prof. Mahaffy[52] has aptly termed them a “tropical Siberia”)
in times when life and labour were cheap, and a very moderate yield
may under those conditions have been satisfactory.[53]
PLATE IV.
[Illustration: Ruins of Um Eleiga. Gebel Abu Dahr in the Background.]
[Illustration: Ruins in Wadi Shenshef.]
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