IN THE ESNA-IDFU REGION, NILE VALLEY, EGYPT 9 



part of the outcrops in the region and are locally unconformably overlain by one or 

 more of the much younger deposits of the Pliocene, Pleistocene and Recent, which 

 constitute the rest of the outcrops in the region (Text-fig. 3). 



Fig. 1. Map of Egypt. 



