Belek
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This breadth was formed during the era of torrential rains occurring afterwards the tectonic phenomena which developed in the deathwatch of the arctic aeon aloft getting abounding with the alluvia agitated by rivers. The charcoal of this era aggregate hillocks covered with ache and heath, accepted as CONGLOMERATE, formed of beach and dust accumulated to a acme of 100 meters. As the rivers connected to backpack the alluvia in the administration of the sea, these albino hillocks remained on the plains and gradually became abroad from the shore. During the endure appearance of the bushing process, continued ridges and cordons consisting of beach and dust were formed forth the bank because of the ample amounts of alluvia agitated by the rivers.
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