=Gebel el Anbat= is conveniently considered here, though it lies on the south side of the Wadi Hodein. It presents a somewhat similar appearance to Gebel Harhagit, from which it lies nineteen kilometres south-east, and like it bears a beacon on its summit. The position of the beacon is latitude 23° 6′ 5″, longitude 35° 19′ 27″. El Anbat is lower than Harhagit, being only 390 metres above sea-level; it consists also of a different rock, being chiefly composed of curious brown and reddish calcareous schists. Gebel el Anbat is practically in the Wadi Hodein, the main channel of which is deviated by its foot-hills so as to pass round the east side of the hill. It is best ascended from the south, where a camp can be fixed about 600 metres south of the beacon and about 255 metres below it; the ascent is easy and occupies less than an hour. Eastward of Gebel Abu Dahr there extends for some thirty kilometres along the south side of Wadi Khoda a mountainous tract of dark rocks, the principal masses of which, from west to east, bear the names of Gebel Hindia, Gebel Um Akra, and Gebel Um Etli. These mountains have only been seen from a distance, and little is known about them beyond the positions and altitudes of their principal peaks, which have been fixed by triangulation. =Gebel Hindia=, thirteen kilometres east of Abu Dahr, rises to 873 metres above sea-level, and is drained partly by the Wadi Hindia to the north, and partly by the Wadi Salib el Azrak. =Gebel Um Akra=, six kilometres further east, is higher, its highest peak, marked by a beacon, being 1,050 metres above the sea, while a ridge a little further south reaches 970 metres; it is drained to Wadi Khoda by the Wadi Um Akra. =Gebel Um Etli=, which forms the south side of the Wadi Khoda just before that wadi emerges on to the coast-plain, has three main summits, reaching respectively to 844, 795, and 764 metres above the sea. It is a rather extensive mass, drained on the north by the Wadis Buluk and Um Lassaf, tributaries of Wadi Khoda, and on the south by the Wadi Um Etli, which reaches the sea independently. =The Faraid Group.= The mountains of this group cover a tract about forty kilometres in length from north to south, between the Wadis Um Etli and Rahaba and lie closer to the sea than any other mountains in the area described, their peaks being only ten to twelve kilometres from the coast. They consist entirely of granite, weathered into a forest of peaks the forms of which render them in respect of shape the most remarkable mountains in Egypt. There are four main masses in the group, of which the three northern ones are called collectively Faraid, while the southern one, which is smaller than, and separated from, the rest, is called by the diminutive name Fereyid.