Geomatic Monitoring Applications to Geomorphological Changes of longitudinal Dunes and their Hazards to Agricultural Development in Suez Canal Lakes Region

Document Type : scientific research and articles

Author

Department of Geography and GIS, Faculty of Arts, Port Said University, Egypt.

Abstract

The Study Area astronomically extends between latitudes °30     ʹ10 and °30   ʹ36 N, and longitudes °32   ʹ15 and °32     ʹ35 E. The area of ​​the region is about 1482 km2. The study seeks to identify the emergence and development of longitudinal dunes, and to examine the extent of their impact on various human uses, specifically the SCLR agricultural lands. In addition, it develops solutions to overcome the hazards of the consequence that the region suffers. The study also attempts to provide solutions that maintain the ecological balance.
    This section focuses on the contributions of the study. It is divided into seven parts: (a) geographical distribution of the longitudinal dunes, (b) morphometric characteristics of the longitudinal dunes, (c) movement of the longitudinal dunes, (d) factors affecting the longitudinal dunes movement,(e) Planted Reins (f) hazards of longitudinal dunes movement on agricultural development, and (g) protection from the environmental hazards related to the longitudinal dunes movement. Each part fathoms out a particular aspect of the research in terms of the data, the procedures of analysis, and the results. As elaborated below, significant elements of each part, if any, are introduced and thoroughly explained.

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Aql, M. T. (2002). Sand Movement East of Suez Canal and its Impact on Human Activity “A Geomorphological Study”, Peer-reviewed Scientific Journal, Faculty of Arts, Damanhour Branch, Alexandria University. -in Arabic-
Bagnold, R.A. (1941). "The physics of Blown Sand and Desert Dunes", Methun, London. P 265.
Cornish, V. (1900)."On Sand Dunes Bordering the Nile Delta". Geol. Journ., Vol.15, London.
Desouki, S. A. (1992). Geomorphology of Sandy Forms in the Basin of Wadi Al-Hajj and Al-Jaddi in Sinai. Arab Geographical Journal, Issue 24. -in Arabic-
Desouki, S. A. (2000). Sand Dunes East of Suez Canal “A Geomorphological Analysis”. Journal of the Faculty of Arts in Benha, Volume VII, Issue 7, pp. 619-696. -in Arabic-
Hajjaj, A. B. S. (2012). Geomorphological Hazards in the Area between Al-Timsah Lake and Head of Suez Gulf, (Unpublished MA Thesis). Faculty of Arts, Cairo University.   -in Arabic-
Imbabi, N. S., & Ashour, M. M. (1985). Sand Dunes in the Qatar Peninsula, Part II. Publications of the Humanitarian Research Center, Qatar University, Doha.- in Arabic-
Khedr, M. M. (2005). Geomorphology of Sand Forms West of Wadi Al-Arish, (Unpublished PhD Thesis). Faculty of Arts, Ain Shams University.-in Arabic-
Mahsoub, M. S. (2004). “Dry Lands”, their Natural Characteristics and their Environmental Problems). Al-Israa Press, Cairo. – in Arabic-