الفهرس 
العنوان : جيومورفولوجية بعض جزر بحيرة السد العالى فى مصر والسودان
الملخصيوجد فقط 14 صفحة متاحة للعرض العام
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المستخلص
phenomena (cuesta) and the forms resulting by wind as (Descendant Duns), And the
third chapter investigated also the geomorphological changes that occur on the Lake’s
islands subjected to (accreted islands of islands with each other, accreted islands of
islands with the banks of the lake), the islands were divided into several islands with
different sizes.
The fourth chapter handled the origin of islands before the establishing the High
Dam through two main points: first, the morphology of the study area before the
establishment of the High Dam and the second, the factors that helped the emergence
of islands in the Lake of the High Dam, represented in the flood, river load,
characteristics of the river bed, the variation of width and slope.
The potential dangers, threats and the development opportunities were analyzed
in the fifth chapter in three points: first, one studied some of major natural dangers to
which the lake is exposed, namely, high evaporation rates and their impacts on the High
Dam’s Lake, the encroachment of sand dunes and their impacts on the Lake. The
accumulation of the Nile silt and its influences on the lake, then the coastal waves,
climatic changes and its threats on the lake, while the second point depicted the impact
of the Renaissance Dam on the High Dam Lake and the third point handled the
available benefits from the High Dam Lake represented in taking advantage of the silt
accumulations, fisheries and tourism activities and opportunities to benefit in the field of
energy.