extended abstracts - Geomorphic Processes and Geoarchaeology
extended abstracts - Geomorphic Processes and Geoarchaeology
extended abstracts - Geomorphic Processes and Geoarchaeology
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<strong>Geomorphic</strong> processes <strong>and</strong> geoarchaeology<br />
engineering-geological drilling. A map of the cultural layer depth was created (fig. 3).<br />
The degree of cultural layer preservation according to the chosen markers is estimated as<br />
high. The verification of the data, gathered by the engineering-geological method, has<br />
begun by traditional archaeological tracing with a trench. A 3.7 m deep trench have been<br />
excavated along the line of the shortened profile <strong>and</strong> preserved till 2012.<br />
The analysis of the l<strong>and</strong>slide section by the archeological trench in 2011 showed a<br />
good condition of cultural layer preservation in the l<strong>and</strong>slide body, despite a long period<br />
of time passed after the destruction. The stratigraphy of the cultural layer is similar to the<br />
one at the settlement (at the excavation area # 7) <strong>and</strong> allows to consider the fragment a<br />
part of the settlement, or a continuation of the cultural layer of the site. It opens prospects<br />
for clear reconstruction of the settlement pattern before it was destroyed by the l<strong>and</strong>slide.<br />
Figure 4. Northern profile of the trench in 2011 on the 4 th generation of the root border<br />
of the Oka river valley<br />
The research also made it possible to carry out more accurate dating as the<br />
l<strong>and</strong>slide itself as well as other natural processes, happening on this territory after the<br />
l<strong>and</strong>slide, track its intensity in different time periods. The data of the research have<br />
proved the preliminary conclusions about the XIV-XVII centuries, as most probable time<br />
of the linear erosion <strong>and</strong> l<strong>and</strong>slide activation. The results still need to be compared with<br />
the existing records of the climate changes at that period.<br />
Research done with the financial support of Russian Foundation for Basic<br />
Research, the project № 11-06-00158-a<br />
References<br />
1. Uskov, V.A., Vodorezov, A.V. 2006. Formirovanie antopogennykh form rel’efa<br />
na istoricheskikh territoriyakh. In: Sklony na istoricheskikh territoriyakh. Ryazan,<br />
RIAMZ, P. 109-116 (in Russian).<br />
2. Vodorezov, A.V., Uskov, V.A. 2002. Izuchenie dinamiki sovremennogo<br />
ovragoobrazovaniya na goroditsche Staraya Ryazan. In: Ekologicheskie problemy<br />
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