Basic Informations

C.V

Languages

Mother tongue: Arabic

Second Language: English

Specialization

Major: Physical Geography .

Specialization: Geomorphology .

Scientific activities and careers :

1. Demonstrator in the Faculty of Arts, University of Beni Suef, 2001 .
2. Assistant Lecturer, Faculty of Arts, University of Beni Suef, 2008 .
3. Work in teaching geography of Africa and the Nile Basin, Geography of transport and trade, geography of seas and oceans, geographical environment, natural geography of Egypt, Geography of the Arab world , faculties of Arts and Education, University of Beni Suef, during the period from March 2006 until now .
4. Member of the Geographical Society of Egypt .
5. Participation in the work of committees of exam preparation .
6. Participation in the supervision of the field study and scientific trips for students of the Department of Geography of the regions: Lake of Karoon and Wadi El Rayan, land use, the new city of Beni Suef, the village of white Arab, North Sinai , Red Sea , Weast Coast Of Egypt , Kharga Oasis .
7. Associate researcher in the study of sand, Egypt rallies , Ain shams University , Desert Research Institute and Heidelberg University(Germany) , 2010-2011 .
8. Associate researcher in the study of environmental loads of 31 industrial zone for heavy industries in Beni Suef , Beni Suef University , 2014 .

Master Title

The Environment of the Nile Islands Located between AL- Hayiba meander in the South and Girza meander in North (A Study in Applied Geomorphology)

Master Abstract

The present thesis is an applied Geomorphology Study of the Nile Islands Located between AL- Hayiba meander in the South and Girza meander in the North. The area being studied is a part of the Nile; it extends along its course from the 71- Km to the 156-Km mark of al-Rawdha Measurement and lies at latitude 28° 46? 30? N and 29° 26? 30? N and longitude 30° 53? E and 31° 15? E. The present study consists of five chapters preceded by an introduction and The introduction includes a display to specify the region and the reasons for choosing the subject, the aims of study and the approaches which has been followed and the study sources and its contents. The chapter I handles the morphological aspects of the studied area in terms of the Nile course as well as the nature of its directions, meanders, and profile. The study revealed that the Nile course in the studied area is sinuous; it consists mainly by many sharp-angled meanders separated from one another by some parts that are almost straight. The general shape ratio is about 81-mm/Km, i.e. 1-m/12,250 Km. Besides, it investigates the birth and formation of some of the studied islands. The chapter II studies the Environmental elements affecting the Nile islands in the studied area though investigating the geological development of the studied area from the early Eocene to the Holocene. It also studies the climatic conditions in a period of 30 years starting from 1967 – 1997. The chapter then presents a detailed study of the soil and natural vegetation. The chapter III examines the morphometric aspects of the islands under study; they are 46 islands and occupy about 18,953 Km. It also investigates the metric aspects of the islands and the relation between such aspects and the processes affecting the islands formation. The chapter IV studies the Environmental changes that the islands were subjected to before and after the High Dam construction. It also deals with the hydrologic changes from the last century until now; and, consequently, some changes in the studied shapes before the High Dam construction. The chapter V is an applied geomorphological study of the islands and the nature of the relation between the various human activities and pollution ratio on these islands. It then evaluates the islands resources and their relation with the Nile and human activities. The conclusion deals present the results of the study.

PHD Title

The Geomorphology of Gabal Ataqa

PHD Abstract

The area under investigation- is a characteristic geomorphological land unit in the N. W of Suez Gulf between lat. 29° 45? - 30° 5 ?N and long. 30° 5 ?- 32° 35 ?Its area is about 857 km2. it aims to study the topographic and geomorphological features, through drawing a geomorphological map to determine the geomorphological agents and processes through which the area of study was formed. The student used regional, systematic, descriptive, and applied approaches, beside the statistical, cartographical, G. I. S., and comparative methods. He depends also on field studies, and laboratory works. The present study consists of five chapters preceded by an introduction and followed by the finality. The introduction includes a display to specify the region and the reasons for choosing the subject, the aims of study and the approaches which has been followed and the study sources and its contents. The first chapter deals with the geology of the study area through studying of the geographical distribution of the geological formations, the stratigraphy, structure and the geological evolution of the studied area and deals with physical characteristics of it. It has been divided into two parts, relief characteristics of the area, its slope and its relief ratio, its general future and dividing it into morphological units distinguish geomorphological characteristics and features. The second part deals with weather and its effect forming geomorphological features. The second chapter deals with the morphometric characteristics of Drainage Basins, such as the area. the Morphometric diminution the form relief, It also deals with morphometric characteristics of the drainage networks in the region through studying the drainage patterns, drainage density and longitudinal profiles. and the relation between the variables of the basins and drainage networks. The third chapter deals with the slope analysis of the study area through studying the general characteristic of Field work measured slope profiles. The slope angles and curvature were and analyzed. The fourth chapter the geomorphological map of the study area was analyzed and geomorphological forms were classified to structural forms, Erosional and deposional land forms. The fifth chapter it deals with the geomorphological hazards as intensive surface run off, sand and mass movement, and the strategies to face their hazards. The conclusion deals with the most important results of the study. The student suggests his recommendations which may contribute to the sustainable development of the study area. The present study also depends on a menu of Arabic and English references and sources.