By H. Stewart Edgell

H. Stewart Edgell is a graduate of the collage of Sydney together with his doctorate in geology from Stanford college. He has spent so much of his operating existence within the heart East, specially in Arabia, the place he has been lively in oil exploration, and essentially in college instructing and study as a Professor of Geology on the Amercian college of Beirut, the UNESCO/Saudi middle for utilized Geology, Jeddah, and King Fahd college of Petroleum and Minerals, Dhahran, Saudi Arabia.
Arabian Deserts presents a accomplished insurance of all of the deserts of Arabia principally in keeping with the author’s event in Arabia during the last fifty years. certain landforms of Arabia deserts are defined, including their geological surroundings and the impact of climates either previous and current. The six nice sand seas of Arabia are emphasised considering that Ar Rub’ al Khali desolate tract types the world’s greatest non-stop sand desolate tract. assets, sedimentology, and the mechanisms of formation of those nice sand deserts are tested. certain sand dunes and interdunes varieties present in Arabia are defined, categorised and defined. Fluvial strategies are mentioned, in addition to the various oases, and lake deposits shaped in milder, extra humid periods. large parts of black, basaltic, volcanic wilderness are defined masking 3 times the world of Belgium. Ecology of Arabia and human effect on desertification are defined. Climatic adjustments within the evolution of Arabian deserts throughout the Quaternary and their motives are defined and a chronology of climatic occasions in the course of their formation is established.
This e-book could be of curiosity to geoscientists, specially Quaternary geologists, geomorphologists, geographers, sedimentologists attracted to aeolian and fluvial tactics, climatologists, coastal reports teams, desertification curiosity teams, and ecologists with curiosity in arid lands.

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Photo by H. S. Edgell). 5. A view of the central Tihamat Asir plain in frequent Acacia in an almost African setting. (Photo by H. S. Edgell). 6. The Tihamat Asir near Jizan with numerous large widyan flowing down to the Red Sea from the Asir Highlands. Farasan Islands (Jaza’ir Farasan) formed by Miocene salt plugs are on the lower left. A typical Red Sea coastal inlet or sharm is seen behind Ras Tarfa near the outlet of Wadi Baysh. Sabkhah areas north of Jizan appear dark. Image width 140 km. pl).

These dunes have an average diameter of 1 km. Image width is 30 km. pl). 5. Linear dunes of Nafud al Ghamis (middle to lower left), including Nafud al Buraydah (lower centre), and Nafud at Tarafiyah (top right). The city of Buraydah is seen to the left of centre. Image width is 30 km centred at lat. 18º N; long. 47º E. pl). 6. Large linear dunes or ‘uruq of the Nafud al Mazhur on the left with minor small linear seif dunes on their surfaces. Giant dome dunes of the Nafud ath Thuwayrat are seen on the right.

20171871120). ‘Uruq as Subay, central part, showing thin, widely spaced, linear dunes or ‘uruq with smaller linear dunes on their surfaces. Image width is 10 km. pl). Dome dunes of the narrow south–eastern Nafud as Sirrah, showing their numerous radiating arms and a finely reticulate surface pattern of smaller dunes on their surfaces. A few NNW–SSE trending linear dunes appear to the south. Image width is 15 km. pl). Nafud Hanjaran and its ENE–WSW trending low ‘uruq lying east of Wadi Bishah with larger ‘uruq NW of Wadi Bishah.

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