255 Archaeological Geology
Tuesday, 7 October 2008
1:30 PM - 5:30 PM
Geological Investigations of a Middle Kingdom Harbor: Wadi Gawasis, Egypt
Paper number: 255-6
Program: Technical Sessions
Time: 2:45 PM – 3:00 PM
Authors
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Duncan M. FitzGeraldBoston University, Boston, MA
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Kathryn A. BardBoston, MA
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Rodolfo FattovichNapoli, N/A
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Chiara ZazzaroNapoli, N/A
Abstract
The base of the corraline cliffs consists of a narrow coral-beach rock platform presently buried by anthropogenic, eolian, and colluvial sediments. A number of occupation sites has been identified within one meter above this beach rock surface. Ubiquitous medium fine wadi sediments are found underlying and beyond the beach rock. Based on sedimentological and malachological analyses, these sediments are interpreted to have been deposited in a tidal lagoon. Mollusk and foraminifera distributions indicate that much of paleo-bay was protected and a low energy environment that received infrequent freshwater inputs. During the time of occupation, the lagoon was closing as wadi processes infilled the bay at rates on the order of .25 cm/year; Mersa Gawasis was likely abandoned due to the rapid infilling of the embayment.