Section of the “Albatross” Quaternary Sediments

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Abstract

The outcrop of quaternary sediments located on the coast of the Kazantip Bay, in the vicinity of the village of Novootradnoye, 300 m south-southeast from the guest house “Albatross” has been studied. The studied continental rocks are probably of eluvial origin. However, a significant amount of sand in their composition may indicate the participation of the deluvial process in their formation — temporary flow associated erosion of bedrock on the uplands located to the south, as well as strong aeolian activity, traces of which are manifested in the form of dusty high-carbonate loess-like loams. The formation of sediments, apparently, occurred during the middle subboreal warming (4800–3400 years ago) and coincides with the period of increasing climate aridization.

About the authors

V. N Komarov

Sergo Ordzhonikidze Russian State Geological Prospecting University

Email: komarovmgri@mail.ru
Moscow, Russia

Yu. A Vaitieva

Sergo Ordzhonikidze Russian State Geological Prospecting University

Moscow, Russia

I. A Goryachev

Sergo Ordzhonikidze Russian State Geological Prospecting University

Moscow, Russia

A. A Dumnova

Sergo Ordzhonikidze Russian State Geological Prospecting University

Moscow, Russia

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