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Toubkal

Highest peak of the Atlas mountain range

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Mt Toubkal
SimonKing74 · CC0

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Through Mountain, Sedimentary rock and Valley

Geography

Although much of the High Atlas consists of sedimentary rocks, the Toubkal massif is an area of volcanic rocks which have weathered into alpine crests, cut by deep, narrow valleys. To the south, the mountain drops steeply down for 1,800 metres (5,906 ft) to a small lake called Lac d'Ifni. To the west, the mountain's edge is marked by a pass, the Tizi n'Ouanoums at 3,664 metres (12,021 ft). From this pass, the mountain's W-S-W ridge rises up to Toubkal West, which forms a shoulder at 4,020 metres (13,189 ft) before continuing to the summit at 4,167 metres (13,671 ft).

The north and western sides of Toubkal drain down to the Mizane Valley, which has the passes of both Tizi n'Ouanoums and Tizi n'Ouagane at its head. Two hanging valleys on the western side of the mountain – the Ikhibi Nord and Ikhibi South – provide ready access for trekkers and climbers to reach Toubkal's summit. At one time the northern valley provided the normal route of ascent, but the construction of a mountain hut by the French Alpine Club below Ikhibi Sud now encourages trekkers to ascend via the southern route instead.

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