| 2005 Salt Lake City Annual Meeting (October 16–19, 2005) | |
| Paper No. 61-9 | |
| Presentation Time: 10:15 AM-10:30 AM | ||
WHAT THE EXCAVATIONS, GEOPHYSICAL & GEOMORPHOLOGICAL INVESTIGATIONS OF ZIYARET TEPE TELL: RESULTS FROM AN ASSYRIAN 'CITY OF CLAY' AT THE EDGE OF EMPIRE | ||
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NICOLL, Kathleen, Centre for the Environment (OUCE), University of Oxford, Dyson Perrins Building, South Parks Road, Oxford, OX1 3QY, England, Kathleen.Nicoll@alumnae.brynmawr.edu, DEMKO, Timothy M., Department of Geological Sciences, University of Minnesota Duluth, Duluth, MN 55812, and MATNEY, Timothy, Department of Classical Studies, Anthropology, and Archaeology, The University of Akron, Akron, OH 44325-1910 Ziyaret Tepe -- one of the few sites in SE Turkey in which cuneiform tablets have been found -- was an important urban centre at the northern frontier of the Assyrian Empire ~900-600 BC. Contemporary and newly translated texts suggest it was the provincial capitol of Tushhan, which was apparently abandoned around the time when Ninevah was sacked by the Medes and the Babylonians ~612 BC. Our geophysical investigations, excavations, and geomorphic surveys have delineated the areal extent of the mounded settlement located on a strath terrace of the Upper Tigris. Subsurface gradiometry maps and a trench at the settlement edge revealed a 6.5m wide city wall made entirely of mudbricks in a casemate fashion. Pilot GPR (ground penetrating radar) surveys ground-truthed unprocessed profiles with excavated features. Assyrian building materials have properties of high attentuation and low transmissivity at the radar frequencies (50 and 100 MHz) and transmitter power (400 V) used. Although observed signal penetration (3-4 m below ground surface) was low, significant larger features were detected. Velocities calculated from CMP (common mid point) surveys reflect the dominant sediment size of geological and cultural materials [0.06-0.09 m/ns; clay-silt, respectively]. Archaeological features with distinctive radar facies include mudbrick walls, baked tiles, set (inlaid) floors, and cobble pavements. However, the signal-to-noise ratio was very low in this environment. Data acquisition suffered artefacts sourced from surface metal objects (e.g. wheelbarrows, horse carts, pipelines), military aircraft, crop furrows, people, and animals (e.g. excavators, shepherds, flocks). | ||
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2005 Salt Lake City Annual Meeting (October 16–19, 2005)
General Information for this Meeting | ||
| Session No. 61 Archaeological Geology Salt Palace Convention Center: 251 F 8:00 AM-12:00 PM, Monday, 17 October 2005 Geological Society of America Abstracts with Programs, Vol. 37, No. 7, p. 155 | ||
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