Clim. Past, 8, 2069-2078, 2012
www.clim-past.net/8/2069/2012/
doi:10.5194/cp-8-2069-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
Possible earthquake trigger for 6th century mass wasting deposit at Lake Ohrid (Macedonia/Albania)
B. Wagner1, A. Francke1, R. Sulpizio2, G. Zanchetta3, K. Lindhorst4, S. Krastel4,5, H. Vogel1, J. Rethemeyer1, G. Daut6, A. Grazhdani7, B. Lushaj7, and S. Trajanovski8
1Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, 50674 Cologne, Germany
2Dipartimento di Scienze della Terra e Geoambientali, University of Bari, Italy
3Dipartimento di Scienze della Terra, University of Pisa, Italy
4Helmholtz Centre for Ocean Research, GEOMAR, Kiel, Germany
5Institute of Geosciences, University of Kiel, Germany
6Institute of Geography, University of Jena, Germany
7Institute of Geosciences & Energy, Water & Environment, Polytechnic University of Tirana, Albania
8Hydrobiological Institute Ohrid, 6000 Ohrid, Macedonia

Abstract. Lake Ohrid shared by the Republics of Albania and Macedonia is formed by a tectonically active graben within the south Balkans and suggested to be the oldest lake in Europe. Several studies have shown that the lake provides a valuable record of climatic and environmental changes and a distal tephrostratigraphic record of volcanic eruptions from Italy. Fault structures identified in seismic data demonstrate that sediments have also the potential to record tectonic activity in the region. Here, we provide an example of linking seismic and sedimentological information with tectonic activity and historical documents. Historical documents indicate that a major earthquake destroyed the city of Lychnidus (today: city of Ohrid) in the early 6th century AD. Multichannel seismic profiles, parametric sediment echosounder profiles, and a 10.08 m long sediment record from the western part of the lake indicate a 2 m thick mass wasting deposit, which is tentatively correlated with this earthquake. The mass wasting deposit is chronologically well constrained, as it directly overlays the AD 472/AD 512 tephra. Moreover, radiocarbon dates and cross correlation with other sediment sequences with similar geochemical characteristics of the Holocene indicate that the mass wasting event took place prior to the onset of the Medieval Warm Period, and is attributed it to one of the known earthquakes in the region in the early 6th century AD.

Citation: Wagner, B., Francke, A., Sulpizio, R., Zanchetta, G., Lindhorst, K., Krastel, S., Vogel, H., Rethemeyer, J., Daut, G., Grazhdani, A., Lushaj, B., and Trajanovski, S.: Possible earthquake trigger for 6th century mass wasting deposit at Lake Ohrid (Macedonia/Albania), Clim. Past, 8, 2069-2078, doi:10.5194/cp-8-2069-2012, 2012.
 
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