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Document Type |
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Project |
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Document Title |
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: Inlets alive Alyssahel geomorphological study of the Gulf of Aqaba Mgartp : الشروم علىساحل خليج العقبة دراسة جيومورفولوجية مقارتة |
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Subject |
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: Inlets alive Alyssahel geomorphological study of the Gulf of Aqaba Mgartp |
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Document Language |
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Arabic |
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Abstract |
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Inlets alive on the shores of the Gulf of Aqaba
Geomorphological study compared
Abstract Search
Specialized research study inlets alive on the shores of the Gulf of Aqaba study geomorphological comparison between eastern coast of the Kingdom of Saudi Arabia and the west coast in the Arab Republic of Egypt, where is the inlets alive a form of interference coastal dry, has been to distinguish between the phenomenon of inlets alive and other interventions coastal similar like Rayyan and bays or estuarine, and was studying geological features of the coastal plains were formed, including inlets alive in terms of geological formations, geological structure of the break-up and structural trends, and then study the origin and geological evolution of the Gulf of Aqaba.
Were studied analysis Morfumtry to Shrum in terms of dimensions of space, height and length of the coast and average breadth and aperture, and formal qualities in terms of form factor and coefficient of elongation and the coefficient of penetration, and to highlight the similarities and differences between the inlets alive on the eastern coast of the Kingdom of Saudi Arabia and the west coast in the Arab Republic of Egypt, miles have been geomorphological study of the properties of the four case studies of Shrum, a Almjop Sharm, Sharm el-Bowl on the east coast in Saudi Arabia, the Negev and Sharm and Sharm El Shaheen Fayyord on the west coast in Egypt, have been classified according to the inlets alive axis direction and geomorphological stage.
Identification of the current study that the inlets alive on the coast of the Gulf of Aqaba have been associated in its inception a concerted set of factors is in the tailings ponds, and erosion of river, and the fluctuation of sea level (the Gulf of Aqaba), the act of coastal processes present, and the sequence evolution geomorphological of Shrum during the time the fourth. |
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Publishing Year |
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1428 AH
2007 AD |
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Number Of Pages |
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53 |
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Added Date |
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Sunday, October 3, 2010 |
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Researchers
| سامية عواد الانصاري | Al-Ansari, Samia Awad | Researcher | Doctorate | sabdulghaffar@kau.edu.sa |
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Files
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27701.doc
| doc | الشروم على سواحل خليج العقبة |
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