<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Poulos, S.</style></author><author><style face="normal" font="default" size="100%">Vassilopoulos, A.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geomorphological and hydrological setting of the touristic beaches of Paros Island.</style></title><secondary-title><style face="normal" font="default" size="100%">1st Conference of the European Federation of Marine Science and Technology Societes (EFMS)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2002</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The flat terrestrial part of the coastal zone of the Paros Island (slope &amp;lt;2,5% for&lt;br&gt;elevations 0-50 m), represents only the 19% of the total area of the island (193 km2). More than 75% of the coastal zone consists of high and lower cliffs, whilst relatively flat and sandy (and/or pebble) beaches do not exceed the 17% of the coastline. The island receives a considerable amount of wave energy; this has its highest values (&amp;gt;1500 W/m) at the NE part of the island and its lowest at the SE “protected” and shallower area. Touristic (sandy/pebble) beaches have been developed along those parts of the coastline that characterized by vulnerable lithology associated with moderate wave activity.&lt;/p&gt;</style></abstract></record></records></xml>