View in Wadi Muelih (Base-line Camp). Gebel Muelih in the Distance.

Granite-boss of Gebel Selaia.

Gebel Iteima is a group of high granite hills rising from the plain fifteen kilometres north of Erf el Fahid. Its highest peak is 849 metres above the sea. It is drained southwards by the Wadi Muelih.

Gebel Hamrat Wogud, which is likewise of granite, is a higher mountain mass fifteen kilometres east of Iteima. Its highest point, marked by a beacon, is in latitude 25° 9′ 34″, longitude 34° 20′ 0″, and 1,103 metres above sea. It is drained southwards by the Rod Um el Farag, a tributary of Wadi Gerf.

Between Gebels Muelih and Mudergeg is a sandy plain with low hills, the more conspicuous of which bear special names; among them are Marwot Rod el Ligah, Erf Sagur, and Khusa el Faraon, the last-named being a group of small but very remarkable black hills eleven kilometres due south of Erf el Fahid. Marwot Rod el Ligah is a triangulation point; its beacon is 514 metres above sea-level.

Gebel Sukari is a very craggy high ridge of granitic rock twenty-two kilometres north of Gebel Zabara. Its highest point, which is at its north end, is 630 metres above sea-level, but the triangulation beacon was erected on a lower part of the ridge further south, in latitude 24° 56′ 50″, longitude 34° 42′ 50″, at an altitude of 476 metres, in order to be near to the extensive old mines and ruins which exist in the locality. Gebel Sukari is drained by various feeders of Wadi Sukari.

Kurdeman is the name of a low hilly district on the east side of Wadi Ghadir, thirteen kilometres north of Gebel Zabara. It is interesting as containing some ancient mines, doubtless worked for gold. A triangulation beacon has been erected on a hill just above the workings, in latitude 24° 52′ 35″, longitude 34° 41′ 35″, at an altitude of 526 metres above sea, or about fifty metres above the wadi.

Gebel Sabahia is a craggy felsite hill five kilometres south-east of Kurdeman, rising to 520 metres above sea, or about ninety metres above the wadi. It is drained by the Wadi Sabahia, a tributary of Wadi Ghadir. In the heads of the Wadi Sabahia, north-east of the hill, are some old gold mines.