Libda sea port has been constructed during Roman Empire, about 2500 years ago. Sea cliffs, sea platforms, wave related furrows and ridges and sea stacks are the most noticeable landforms which resulted from the erosion of the shore. The determined orientation of the equilibrium shoreline is N67W-S67E.
Sand bar blocked the access canal of the port and the rotation area was completely dumped. The beach sediments range in size from coarse to medium sand. Beach rocks were also observed at the sites with groundwater has relatively higher bicarbonate content along the hinter coastal area.
تاريخ النشر
30/05/2006
الناشر
Journal of environmental sciences , the university of Mansoura – Egypt
علي يوسف عكاشة | Aly Y. Okasha | 11219