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Lebanon's tectonic history is closely related to the Levant Fracture System, a left-lateral strike-slip fault zone, separating the Arabian Plate from the African Plate.The intracontinental Palmyride fold belt, with a maximum elevation of 1,385 metres (4,544 ft) above sea level, is an important structural feature that dominates much of Lebanon and Syria, extending northeast towards the ...
In Pennsylvania, the valley is known by three names: (listed from north to south) the Lehigh Valley, the Lebanon Valley, and the Cumberland Valley. Rocks that characterize this region include: limestone, dolomite, slate , shale, sandstone, siltstone, and some scattered basalt.
The Lebanon Valley is part of the much longer Great Appalachian Valley, also called the Great Valley, a natural lowland route running northeast–southwest and lying just inland from the Blue Ridge Mountains and South Mountain. The Great Valley, including the Lebanon Valley, has historically been admired for its fertile agricultural land.
South Mountain is a colloquial name applied to an Appalachian Mountain range extending north and northeast along the south side of Lebanon Valley to the Lehigh Valley region of eastern Pennsylvania. South Mountain includes the southernmost cluster of peaks that straddle Berks , Lancaster , and Lebanon counties [ 2 ] and the northernmost end of ...
Geologic formations of Lebanon (1 C, 2 P) Fossils of Lebanon (40 P) P. Paleontology in Lebanon (1 C, 6 P) Pages in category "Geology of Lebanon" ... Great Rift Valley; H.
Most of Lebanon's rainfall is in the four months of winter, but over the last 45 years, the Ministry of Environment (Lebanon) estimates that rainfall has decreased overall between 5 and 20 percent. [10] The coastal strip of Lebanon gets approximately 2,000 mm of rain per year, while the Beqaa Valley to the east gets only one-tenth as much. [11]
19th century map of Lebanon and northern Palestine with modern and ancient names of rivers. This is a list of waterways named as rivers in Lebanon.Lebanon has 22 rivers all of which are non-navigable; 28 rivers originate on the western face of the Lebanon range and run through the steep gorges and into the Mediterranean Sea, the other 6 arise in the Beqaa Valley.
It is the largest artificial lake in Lebanon, located in the southern part of the fertile Beqaa Valley, with a total capacity of about 220 × 10 ^ 6 m 3 (0 × 10 ^ 9 cu ft) and effective storage (live storage) of 160 × 10 ^ 6 m 3 (0 × 10 ^ 9 cu ft). The power generation is a primary benefit, which meets about 7%–10% of the power ...