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2 edition of geography and geology of the district between Gebel Ątâqa and El-Galâla El-Baharîya (Gulf of Suez) found in the catalog.

geography and geology of the district between Gebel Ątâqa and El-Galâla El-Baharîya (Gulf of Suez)

Hassan Sadek

geography and geology of the district between Gebel Ątâqa and El-Galâla El-Baharîya (Gulf of Suez)

by Hassan Sadek

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  • 27 Currently reading

Published by Government Press in Cairo .
Written in English

    Subjects:
  • Geology -- Egypt -- Suez,
  • Physical geography -- Egypt -- Suez,
  • Geology, Stratigraphic -- Tertiary.

  • Edition Notes

    Statementby H. Sadek.
    SeriesSurvey of Egypt paper -- no. 40
    The Physical Object
    Paginationviii, 120 p., [1] folded leaf of plates :
    Number of Pages120
    ID Numbers
    Open LibraryOL18826748M

    ISBN Published by CPGS, 24 October £ Colour: pp. despite the fact it contains some of the most varied and fascinating Carboniferous geology to be found anywhere in the country. Thus, we can thank Paul Kabrna for assembling a team of experts to produce the first book to specifically focus on the geology of. Garara structural graben is the most pronounced Phanerozoic rock inlier in the Precambrian exposures of Egypt. Many workers referred to Garara graben as the biggest one of the NW structural grabens bordered by deep-seated faults of the Red Sea trend in the Eastern Desert of Egypt in the North East African Shield, e.g. Schurmann ().It extends in the Southeastern Desert from Kom Ombo (40 km.

      Wadi El Khariq has a vast area that can be reclaimed. Upper Jurassic carbonates represent the main aquifer. The Desert Research Center has a pilot station in Wadi El Khariq that suffers from water deficiency. Therefore, the drilling of new wells is needed. As fault zones make fracture conduits for groundwater, detecting these faults is a vital process. Therefore, this study aims to trace . The Geography of Georgia: Problems and Perspectives (World Regional Geography Book Series) eBook: Bondyrev, Igor V., Davitashvili, Zurab V., Singh, Vijay P.: Amazon.

      Wadi Wurayah area is one of the major wadis originating and running on the Oman Mountains and drains into the Oman Gulf. These wadis in general and Wadi Wurayah in particular are characterized with a rich diversity of rare and mountainous and freshwater habitats and species. These wadis contain unequal, representative, and sensitive areas of the dry lands ecosystem with natural, Cited by: 1. Geography 3 or 4 or 6 (Cultural Geography, Globalization, or World Regions) Statistics 12 (Statistical Methods for Geography and Environmental Studies) The Major (11 courses - 44 units minimum) To declare, students must have completed TWO (2) Geography course at .


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Geography and geology of the district between Gebel Ątâqa and El-Galâla El-Baharîya (Gulf of Suez) by Hassan Sadek Download PDF EPUB FB2

The Geography and Geology of the District between Gebel Ataqa and El-Galala El-Bahariya (Gulf of Suez) Hardcover – by H Sadek (Author) Be the first to review this item. See all formats and editions Hide other formats and editions. Price New from Author: H Sadek. Get this from a library.

The geography and geology of the district between Gebel'Atâqa and El-Gal-ala El-Baharîya (Gulf of Suez). [Hassan Sadek; Misāḥah al-Jiyūlūjīyah al-Miṣrīyah.]. Geology of gebel 'El'Ineigi' District. [G A Moustafa] on *FREE* shipping on qualifying : G A Moustafa. Sadek, “The Geography and Geology of the District between Gebel Ataqa and El Galala El Bahariya (Gulf of Suez),” Egypt Survey Department, Cairo, 被如下文章引用: TITLE: Seismicity and Geologic Structures Indubitable in Wadi Hagul, North Eastern Desert, Egypt.

Gebel EI-Dist. which lies near the northern scarp of the Bahariya Oasis (Figure 1), is considereLi to be the type section of the Bahariya Formation (Lower Cenomanian). The latter represents the oldest exposed rocks in the area and is unconformably covered by Eocene limestones and by: 1.

The study of eight stratigraphic sections along Cairo–Suez district, between Gebel Ataqa and Gebel Mokattam, reveals a thick Lower Eocene Ypresian carbonate section, approximately m thick, at Gebel Abu Treifiya just to the west of Gebel Ataqa.

It is represented by the Minia Formation rich in Nummulites praecursor, Orbitolites pharaonum Schwager, Alveolina frumentiformis Schwager, and.

The age of Malha Formation that located at Gebel Sarbut el-Gamal in the southwestern Sinai is a controversial point, due to the absence of index fossils. archaeology, forestry, geography, geology and others. According to the United Nations (95th Plenary meeting, 3rd December, ), Remote Sensing means sensing of earth’s surface from space by making use of the properties of electromagnetic wave emitted, reflected or diffracted by the sensed objects, for the purpose of improving naturalFile Size: KB.

Report of the Sixth International Geographical Congress: Held in London,Issue 6. Hugh Robert Mill. Murray, - Geography - pages. 0 Reviews. Preview this book. Geology The Central Depression (Fig. 1 b) is a result of the forearc movements and the uplift of the Andes to the east. The Central Depression infilling occurs during the late Cenozoic by non-marine siliciclastic deposits and pyroclastic flows (up to m thick).

Geology The Bala Fault is a south-west to north-east trending geological fault in Wales that extends offshore into Cardigan Bay. The resulting valley is occupied by the town of Bala, Bala Lake (Llyn Tegid) and further south and east by Tal-y-Llyn and the Mawddach Estuary.

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It is the commercial capital of India and a global financial hub. It has been the main seaport in the Arabian Sea since the opening of the Suez Canal. The Jawaharlal Nehru Port of Mumbai handles 60% of India’s containerised seaborne Size: KB.G21 Region geography This profile provides Census data for the G21 Region broken down into small areas based on customised suburbs/localities.

For the, and Census years these small areas are created by aggregating Census Collection Districts.INTERNATIONAL JOURNAL OF SCIENTIFIC & TECHNOLOGY RESEARCH VOLUME 4, IS OCTOBER ISSN IJSTR© composed of shale intercalated with sand and gravel, the Asu River Group (sand, sandstone and gravel).

Nkporo-Afikpo shales formation is made up of sands, sandstone, intercalated.