*1.2.6. Mit Ghamr formation (Late pliocene)*

Mit Ghamr Formation consists of thick layers of sand and pebbles which show clay interbed‐ dings of limited thickness. The depositional environment of this formation is probably shallow marine to fluvial. It is a typical fill-up basin with coastal sands, coquina beds, clay and peat. It conformably underlies the Bilqas Formation.
