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ESSAY No 1
CUESTA FEATURES IN THE LEBANON MOUNTAINS 5394
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Abou el-Enin Ajaltoun Albian alluvial fans Anti-Lebanon Mountains Anticline Aptian area under consideration Baakline bands Bathonian Batroun beds Beirut Beirut Arab University Beskinta break of slopes cave of Jaieta Cenomanian limestone Chekka cliff-line Cretaceous Dahr debris deeply incised developed dip-slope doline dolomite Dubertret east eastern El-Bekaa Plain El-Modairej erosion surface remnants examined fault scarp Feitroun Field investigation flattish floor formations geomorphological Glaciation head of Nahr heavily jointed height isolated hills Jebel Jezzine Jurassic Jurassic limestones Karst areas Karst features Karst forms landslides Lebanese coastal plain Lebanon Mountains Lebanon Mts Liban lithology lower major cuestas mapped marine terraces marls metres O.D. morphological Nabeh Nahr El-Kelb noted occur periglacial Plate Pleistocene polje Qadicha Qanat relatively rocks sandstones scarp-slope shales side of Nahr sinks slide masses slide ridges soliflual solifluction deposits southern stage stalagmites steep streams surface forms thick Turonian type II solifluction valley sides vary Vaumas village Yammouna depression