Eleven Samples of costal sand was studied, nearly south- north along 15 km ,27
Spcieses of Foraminifera Testes was determined (founded)in it, most of them was benthic ,
but the porcelanic testes were more commen.
This Costal sand is richer in Fora
minifera Testes near the costal line. As well as the
fine far costal sand less richer in Foraminifera Testes than the coarse sand which is near of
costal line, because of the effect of weathering , which the Aeolian processes very clear in
it. And this causes brokig the Foraminifera Testes.
The recent geological processes can be reflex at the past geological time, especially
for sand stone in Pleistocene Age. This sandstone deposit by geological processes
seemlywhat happing in our days ( recent).
