Geoarchaeological Interpretations of the “Trojan Bay”
Geoarchaeological Interpretations of the “Trojan Bay”
复制标题
“特洛伊湾”的地质考古学解释
DOI：
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发表时间：
2003
期刊：
影响因子：
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通讯作者：
S. Vardar
中科院分区：
文献类型：
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作者：
I. Kayan;Ertuğ Öner;Levent Uncu;Beycan Hocaoǧlu;S. Vardar
全新世期间海平面上升，在Karamenderes （Scamander）河谷下部形成了一个ria型海湾（Troian bay）。大约在7000-6000年前，在现在的平原以南17公里处。从那时起，冲积作用和三角洲沉积作用使恰纳卡莱海峡（达达尼尔海峡）的海岸线向北移动。在青铜时代，海平面相对下降了2米，加速了这一过程。因此，特洛伊最初是一个沿海定居点，而在第四，第五和第六时期，西部地区是一个广阔的三角洲沼泽。卡拉蒙德勒斯三角洲平原沿海地区海水非常浅，整个退化期陆地都被沼泽覆盖。因此，地理环境从来不适合建立一个重要的港口或以港口活动为基础的城市发展。
Sea-level rise during the Holocene brought about a ria-type bay (Troian Bay) in the lower part of the Karamenderes (Scamander) valley which intruded approx. 17 km up to the south of the present plain about 7000–6000 years ago. Since then, alluviation and deltaic progradation has moved the shoreline north of the Canakkale Strait (Dardanelles). A relative fall in sea level of about 2 m in the Bronze Age accelerated this process. Thus, Troia was a coastal settlement at first, while the area to the west in periods IV, V and VI was a broad deltaic swamp. The sea in the coastal zone of the Karamenderes delta plain was very shallow, and the land was covered by swamps during the entire progradation period. Therefore, the geographical environment has never been suitable for the establishment of an important harbour or city development based on harbour activity.