Belek
May 22nd, 2008 admin
This area developed in a time of, flooding rains developing following tectonic developments after the ice age and thus as consequence of the washing country, which the rivers had angespült. From this time hills stayed, which solidified themselves up to 100 m highly, of gravel and sand to be consisted, today as a conglomerate designated and with Pinienwäldern and Gestrupp bewachsen are. Fliebenden waters continued with the time toward sea, meanwhile them far washing countries anspülten, and as consequence of it the sand hills remain within the level and ever further from the sea. Due to these enormous washing ashore of the rivers oblong developed, from sand and gravel existing hill backs and deposit strip in the last phase of the replenishment process along the coast. Therefore the rivers, which were handicapped in their river thus and found no direct entrance more to the sea, formed toward the east and behind the hill backs running sheet, until they flowed then in the sea. In the north of the area near Gebiz the Uçansu of Wasserfalle (“itself evaporating Wasserfalle”) are and in the proximity of the village Akbaş the Zeytintaşı cave (olive stone cave) at the settlement area, which is with their Stalaktiten and Stalagmiten beautiful and very fascinating. Behind the coastal strip of the area around Belek the place Kadriye with numerous holiday areas, purchase possibilities and any kind of tourist activities lies. At the beaches of Kemerağzı, Belek and Serik are the most modern tourism plants. The proclamation and marketing of these holiday areas on highest, international level are made by the together created federation of the plants with names BETÜYAP. Also the Pinienwälder of the environment grown closely offers a particularly beautiful sight. Further the area has six gulf clubs with 19-Loch-Plätzen on international level and pertinent hotels.
