Creation and destruction of travertine monumental stone by earthquake faulting at hierapolis, Turkey
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Published:January 01, 2000
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CiteCitation
P. L. Hancock, R. M. L. Chalmers, E. Altunel, Z. Çakir, A. Becher-Hancock, 2000. "Creation and destruction of travertine monumental stone by earthquake faulting at hierapolis, Turkey", The Archaeology of Geological Catastrophes, W. J. McGuire, D. R. Griffiths, P. L. Hancock, I. S. Stewart
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Abstract
The presence of travertines adjacent to the city and their value for construction was well known to the Greek, Roman and Byzantine residents of Hierapolis (modern Pamukkale). The travertines were mainly extracted from quarries on the outer slopes of a low plateau below the city. The distinctive attribute of most of the quarries is that they are narrow but deep vertical-sided trenches. Each trench is the site of a nearly vertical fissure that was filled by banded fissure travertine, one type of so-called Phrygian marble. Trench walls, formerly the contacts between vertical banded travertines and outward dipping bedded travertines,...
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Contents
The Archaeology of Geological Catastrophes

Archaeology is playing an increasingly important role in unravelling the details of geological catastrophes that occurred in the past few millennia. This collection of papers addresses both established and innovative archaeological methods and techniques, and their application in examining the impact of earthquakes and volcanic eruptions. This comprehensive volume includes case studies from around the world, such as Europe, Africa, SE Asia, Central and North America; covering historical and archaeological aspects of earthquakes and volcanic eruptions.
Although the bulk of the collection views earthquakes and volcanic eruptions as agents of destruction, the volume also considers their potential benefits to past cultures - providing materials for tools, building and sculpture, and even the fertile environmental conditions on which societies depended. New geophysical, geological, and archaeometrical methods and techniques are described and the application of these new ideas presented, providing improved knowledge of these ancient catastrophes. There is a strong focus on arguably the most prominent geological catastrophe in the archaeological record - the Bronze Age eruption of Thera (Santorini, Greece) and its consequent regional impacts on Minoan culture. This multidisciplinary text is of benefit to academic researchers and educators in archaeology, palaeoseismology and volcanology alike.