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Bu araştırma Teos antik kenti çevresinde Holosen boyunca meydana gelen kıyı çizgisi ve doğal çevre değişmelerinin belirlenmesi amacıyla yapılmıştır. Antik kentin çevresinin paleocoğrafya koşullarının ve bunun jeoarkeolojik sonuçlarının belirlenmesinde alüvyon delgi sondaj yöntemi kullanılmıştır. Teos antik kenti kıyıya paralel uzanan K-G doğrultulu Ekmeksiz tepe sırtının doğu güneydoğu yamacı ile etekleri boyunca geniş bir alana yayılmıştır. Yapılan 11 delgi sondaj kentin doğusundaki Çayırarası kıyı ovasında K-G ve B-D doğrultulu iki hat üzerinde yapılmıştır. Paleocoğrafya ve jeoarkeoloji değerlendirmeleri sondaj örneklerinin sedimantolojik, element ve mikropaleontolojik analizleri yapıldıktan sonra elde edilen verilere dayanarak yapılmıştır. Elde edilen ilk bulgulara göre Çayırarası kıyı ovası dolgularının katmanlarının en alttan en üste doğru denizel ortam sedimanları, kıyı bataklığı ortamı, Çayırarası taşkın ovası ve Teos kültür dolgularından meydana geldiği belirlenmiştir. Teos-2019-01 sondajından yapılan C14 tarihlemesi GÖ 3320 (Calibrated) yılını vermiştir. Buna göre, Çayırarası ovasının bulunduğu depresyonun Orta Holosen’de (Nortgripiyen) (Erken Tunç Çağı) K-G doğrultusunda uzanan boğaz şeklinde bir deniz ve Teos antik kentinin üzerinde bulunduğu Ekmeksiz tepenin bir ada olduğu saptanmıştır (GÖ 7000-6000). Teos antik kenti ve limanının Çayırarası depresyonuna uzanan kesiminin Tunç Çağı’ndan günümüze Yassıçayın taşkınları ve yamaç selleri ile örtüldüğü belirlenmiştir.
This research was done with the aim of identifying the coastal lines and natural environmental changes that occur around the ancient town of Theos along the Holosen. For the determination of the paleocographical conditions of the surrounding city and its geoarchological consequences, the method of allyvian dust extraction was used. The ancient town of Teos, which extends parallel to the coast, is spread to a wide area along its edges with the east and southeastern edge of the K-G-directed breadless hill back. The 11 hole exploration was carried out on two lines in the K-G and B-D direction in the eastern part of the city. Paleocoreography and geoarcheology assessments were made on the basis of data obtained after the sedimantological, elementary and micropaleontological analysis of the sonding samples. According to the first findings obtained, the layers of the intercontinental coastal oval fillings are determined right in the bottom; the marine environment is derived from the sediments, the coastal coastal environment, the intercontinental coastal oval and the Teos culture fillings. The date of the C14 from the Teos-2019-01 survey has given the year 3320 (Calibrated). According to this, it was found that the depression in which the inter-cover is located is a sea in the form of a throat that stretches in the middle Holosen (Nortgripien) (The Early Tune Age) in the direction of K-G and an island of the Unclean Mountains located above the ancient town of Theos (E.C. 7000-6000). The ancient town of Theos and the port extending to the inter-depression section has been determined to be covered by the Yassıçay's strawberries and the strawberries from the Tunç Age to the present day.
This research was carried out to determine the changes to the coastline and to the natural environment that occurred during the Holocene Epoch around the ancient city of Teos. Alluvial core drilling method was used to determine the paleogeographic conditions of the ancient city and its geoarchaeological results. 11 core drillings were carried out on two lines in the K-G and B-D direction on the coastal plain of Çayırarası in the east of the city. The paleogeography and geoarchaeology evaluations were made based on the data obtained after the sedimentological, element and micropaleontological analyzes of the drilling samples. According to the first results, the layers of the coastal plain fillings of Çayırarası are marine sediments, coastal swamp environment, Çayırarası flood plain and Teos culture fillings. C14 dating from Teos-2019-01 drilling determined the year to be 3320 BP(Calibrated). Accordingly, it was found that the depression in the Çayırarası plain was a strait-like sea extending towards the K-G direction in the Middle Holocene and that the Ekmeksiz hill where the ancient city of Teos was located was an island. Our findings determined that the section of Teos antique city and harbor extending towards the Çayırarası depression had been covered with floods of Yassıçay and slope floods since the Bronze Age.
Field : Sosyal, Beşeri ve İdari Bilimler
Journal Type : Uluslararası
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