05.05.2013 Views

extended abstracts - Geomorphic Processes and Geoarchaeology

extended abstracts - Geomorphic Processes and Geoarchaeology

extended abstracts - Geomorphic Processes and Geoarchaeology

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

<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 />

274

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!