Abstract
ABSTRACT A purely graphical and descriptive study is carried out of the results of the mechanical analysis of aeolian sand samples from five aeolian microenvironments of the Suez Canal Zone. These microenvironments are shown to differ by small but significant amounts. Taking into account the geographical environment, the results are found to agree with a deduction from Bagnold's Theory of Saltation, allowing for the effects of grain size variation of the materials taking part in the process.
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