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Morphoemtric Study (Al kandeelWadi Basin)

حوض وادي القنديل (دراسة مورفومترية)

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 Publication date 2009
  fields Geography
and research's language is العربية
 Created by Shamra Editor




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The basin of Al-Kandeel Valley represents one of the basins of western northern area's mountains in the Syrian Arab Republic which is situated just like the axe in the eastern northern and western southern direction covering approximately 155km2 with a length rating 20km of complicated geology character (Structurally & Constructively) where you can find a variety of surface rocks among of which there are metamorphic and sedimentary rocks that are of severe dislocation as being subject of high construction potential imposed by the location of the area under the aspect of thrust of the Arab plate under the Jurassic plate. Its height is gradually rating clearly from the eastern northern to western southern. The values of its local terrain rated between 5 m/km2 in its plain area at the drain point and 375 m/km2 at the mountain eastern northern area. The climate prevailing in this area is of seasonal rains and classified under the Mediterranean Climate (Plain-Mountain).



References used
حاج حسن، محمد فائد، ( 1996 ): أسس الجيومورفولوجيا المناخية، منشورات جامعة دمشق، دمشق.
حسين، كمال محي الدين ( 1998 ): جيولوجية سورية الإقليمية ( 2)، منشورات جامعة دمشق، دمشق.
Chorley, R,J; (1962): Geomorphology and General Systems Theory , in King, C.A.M; (ed): (1976): Landforms and Geomorphology Concepts History, Dowden &Ross .Inc .Pennsylvania , PP 238-244
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The obtained results by hydrogeological and Tectonic survey related to fresh water resources in Al-Sin Basin, indicated that the fundamental aquifer of underground water in AL-SIN region belong to Jurassic. The alimentary basin of Al-Sin spring depen d upon filtration of rainfall water and snow throw Jurassic formation from north and north–east of basin. Direction of underground water circulation is toward west and south-west where we find flow place of Al-Sin spring and submarine fresh springs near seashore. Tectonical study shows the existence of fractures and fault groups with NE-SW, ENE-WSW and NW-SE directions. Groundwater movement has the same direction of fractures and faults NE-SW to ENE-WSW and Al-Sin fault structure which allow the existence of direct relation between principal Jurassic aquifer and secondary aquifer especially Cenomanian one.
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Study of the general characteristics of Fractures in the central part of the AL-Kabir AL- Shimali river basin showed the presence of several main groups of Fractures with directions NE-SW _ NNESSW, NW-SE , E-W.and showed increased fracture rate in the northern and southern parts of the study area, and that the spacing between the Fractures close to the medium convergence (5-34) cm , also show a aperture ranged between (0.1-5.1) cm, where aperture width was increased in southwest of Lake 16 October near Lattakia- Kless fault .

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