Aksenov А.О.1,2,3, Rybalko А.Е.2,4, Fedorov G.B.5, Sergeev А.Yu.1, Moskovtsev А.А.1

RELICT COASTAL FORMS ON THE BOTTOM OF LAKE LADOGA AND THEIR CONNECTION WITH HOLOCENE REGRESSIONS 

Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 10.

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doi: 10.24412/2687-1092-2023-10-314-317

Лицензия Creative Commons

1 A.P. Karpinsky Russian Geological Research Institute, St. Petersburg, Russia

2 Saint-Petersburg State University, St. Petersburg, Russia

3 Arctic and Antarctic Research Institute, St. Petersburg, Russia

4 VNIIOkeangeologia, St. Petersburg, Russia

5 A.L. Takhtajyan Institute of Botany NAS RA, Yerevan, Armenia 

 

     

Abstract. This study is dedicated to the analysis of seismic acoustic data for the purpose of reconstructing the positions of Lake Ladoga shorelines during periods when its level was lower than present. Within the scope of this work, archive data from echo-sounding and modern materials of acoustic profiling have been used. Landforms that mark the position of the shoreline at various depths, such as coastal ridges, bars, terraces, and river deltas, have been identified. Paleoshorelines at depths of 12-15 m and 20 m have been reliably established. It is hypothesized that the maximum regression of the lake reached depths of 35-40 m, which is indicated by erosional truncations on the surface of glacial lacustrine sediments and buried erosional incisions made in glacial lacustrine deposits.

Keywords: Lake Ladoga, the Holocene, water-level fluctuations, acoustic profiling, coastal forms

 


 

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Cite this article:

Aksenov А.О., Rybalko А.Е., Fedorov G.B., Sergeev А.Yu., Moskovtsev А.АRelict coastal forms on the bottom of Lake Ladoga and their connection with Holocene regressions // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2023. Issue 10. P. 314-317. doi: 10.24412/2687-1092-2023-10-314-317

 

 


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