Abstract:

Turkey, especially the western Anadolu or the Egean coast, has been the scene of important settlements because the geographical conditions have been favorable throughout the history. With the rise in the sea level of these settlements developing in the coastal areas in Holosen, the natural environments have changed significantly. The settlement history of the Damlıboğaz and Rizav mountain in the Sarıçay valley, which is opened to the Gulf of the West of Anadolu, extends to the Tunç era and the natural environment of that period is different from today. Located in the west of the centre of the Milas County, the Sarıçay oval is a tectonic depression base formed by the alivions of the same name stream. Rice is located on the south-eastern edge of this alivial depression as an output to the mountain. There are archaeological remains on the roof and on the oval area on the roof and on the roof. The ancient settlements in Sarçay Depression and the Rice Mountain have changed their natural environments considerably since their first establishment to this day. The determination of how much the coastal line is most put into, whether or not it reaches the river hill, and how far it progresses most in the north of the Sarıçay valley, and the ancient Gulf coastal line and sea level changes are important questions in this area. In order to determine the paleo-geoarchological characteristics of the grapefruit and the river mountain surroundings, in the alivial area in early September 2016 5 holes were drawn out. In the 3 explosions between the Gulf of Rose and the Rice Mountains, when it dropped from the surface to the present sea level, the sea has been reached to the seafood. According to this, it is clear that the sea is driven up to the rocks of the rice mountain. In the north of the Sarıçay oval and in the oval area in the front of the Damlıboğaz village, in the 2 sondages, archaeological remains were found when they dropped from the surface to a depth of 5 meters. They are the ones that are deeper and deeper in the water. It is probably clear that the rest of the coast, which is northward in the period when the sea level rises and is put into the depression of Sarıçay, is also developed in submarine environments.

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