Satellite image of Lebanon showing snow-covered prominences
The
geomorphology of
Lebanon consists of the coastal plain, the western mountain range (
Mount Lebanon), an interior valley (the
Beqaa Valley), and the eastern mountain range (the
Anti-Lebanon). The Mount Lebanon range stretches from the northern region of Jabal Akkar southward, reaching elevations of 3,088 m (10,131 ft) at
Qurnat as Sawda, Mount Makmel's highest peak, down to 1,091 m (3,579 ft) in
Jabal Niha. The hills of Jabal Amel begin after Jabal Niha.[1] This total length of the Mount Lebanon range is 160 km (99 mi) with a width ranging from 45 km (28 mi) in its northern section, and 25 km (16 mi) in its central part. Numerous smaller hills that create a transitional zone between the sea and the peaks. The western face of the Mount Lebanon range features a series of narrow valleys that run parallel to each other, sloping westward towards the sea, and channeling various watercourses. The eastern slopes descend toward the Beqaa Valley and are steeper compared to their western counterparts. During winter, a few seasonal rivers emerge from the eastern face snowmelt.[2][3]
The Anti-Lebanon mountain range begins in
Yanta and ends in
Shebaa, and measure more than 100 km (62 mi) long and 30 km (19 mi) wide. Unlike Mount Lebanon, the Anti-Lebanon is devoid of deep valleys.[2] This page contains a sortable table listing mountains of Lebanon in both the eastern and western mountain ranges.
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"Mlikh" [Mlikh: A Preliminary Historical Study]. ARAM Periodical (in French). 15. Oxford: ARAM Society for Syro-Mesopotamian Studies: 275–286.
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Environment and Ecology in the Mediterranean Region. Cambridge Scholars Publishing.
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