19892

Hierapolis'teki arkeosismik hasarların değerlendirilmesi

Hierapolis antik kenti, Gediz grabeninin güneydoğu ucunun kuzey kenarını sınırlayan Pamukkale fayı üzerinde yer almaktadır. Hierapolis, antik çağlarda birçok depremden hasar görmüştür, ancak bunlardan en önemlisi M.S. 60 yılında meydana gelmiştir. Bu çalışmada ele alınan önemli iki noktadan birincisi, Hierapolis antik kenti içinde Roma ve Bizans dönemine ait yapıları etkileyen yüzey kırıklarını detaylı olarak incelemektir. Bu yüzey kırıkları kent içinde ve çevresinde yaklaşık 1250 m takip edilmektedir. Yüzey kırıklarının uzunlukları 10 cm ile onlarca metre arasında, genişlikleri ise birkaç milimetre ile 1 m arasında değişmektedir. Yüzey kırıkları boyunca düşey ve yanal yerdeğiştirmeler de mevcuttur. Yüzey kırıkları incelendiğinde, kırıkların oluşmuna neden olan depremin 6.0

Evaluation of archaeoseismic damages at hierapolis

The ancient city of Hierapolis is situated on the Pamukkale fault which bounds the northern margin of the Gediz graben in its south - eastern end. Hierapolis was damaged by many earthquakes in historical times but the most damaging one was in 60 AD. One of the main objective in this study is, detailed investigation of surface ruptures that damage Roman and Byzantine buildings within the ancient city of Hierapolis. Surface ruptures within and near Hierapolis can be traced along about 1250 m. Surface ruptures vary in length from 10 cm to tens of metres and they vary in width from vefew millimetres to about 1 m. There are also normal and lateral displacements along them. As a result of detailed investigation, it is concluded that these surface ruptures at Hierapolis formed during an earthquake with magnitude 6.0

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