الفهرس 
CHAPTER I. - INTRODUCTION.Only 14 pages are availabe for public view
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Abstract
The area east of Beni Suef and Minia is characterized by the pr the exposed Eocene plateau which composed mainly of Middle E in the southern part and the Middle Eocene and Upper Eocene in the part of this area. The area is dissected by two very large drainag known as Wadi Sannur in the north and Wadi EI Sheikh in the so area is characterized by the presence of many naturally economic r that represent the mam income of the Beni Stratigrapically, Sannur Formation could be differentiated into two separated by regionally amalgamated unconformity surface demar development of deep paleokarst profile. The rocks exposed in the tributaries of wadi Sannur are characterized by abundance of carbonat sequences of Middle and Upper most Middle Eocene age. Few occu of Quaternary sediments are represented by the main terraces extending the different tributaries of the Wadi Sannur.
The thesis is considered an applied study for one of the very high and exceptional economic value with an overview environmental impli It has a good recommendation for a better understanding for the fo and localization of the ”Egyptian Alabaster” ”Boutchino”, ”Sylvia” in the Gabal Sannur and surrounding areas.
The geomorphologic studies indicate that the area of Wadi Sannur Protectorate is located in area characterized by development of ideal features and karst deposits. These karst terrains are developed depend~ the interaction of fresh water draining the area through different dr’ basins running within the present study area.