<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Tzalas, C.</style></author><author><style face="normal" font="default" size="100%">Zerefos, C.</style></author><author><style face="normal" font="default" size="100%">Repapis, C</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geomorphological and Archaeological Features of Alexandria Depicting Subsidence of the Coastal Zone.</style></title><secondary-title><style face="normal" font="default" size="100%">Enalia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;The littoral region of Alexandria, east of Silsileh (the eastern promontory of the Eastern&lt;/div&gt;
&lt;div&gt;Harbor) to Montazah promontory was investigated combining archaeological and&amp;nbsp;geomorphological evidence in order to better understand the subsidence of the coastal&amp;nbsp;zone. The coastal zone is rich in archaeological and geomorphological features able to&amp;nbsp;provide insights into the evolution of the coastline and the relative sea level changes. Our&amp;nbsp;study has revealed a continuous subsidence of the coastal zone, owed to various&amp;nbsp;contributing processes, while further research is required to decipher the coastal evolution&amp;nbsp;of this littoral.&lt;/div&gt;</style></abstract></record></records></xml>