The Balkans: glacial landforms during the Younger Dryas Stadial

Book chapter


Hughes, P.D., Allard, J., Woodward, J. and Pope, R. 2022. The Balkans: glacial landforms during the Younger Dryas Stadial. in: Palacios, D., Hughes, P. D., García-Ruiz, J. M. and Andrés, N. (ed.) European Glacial Landscapes: The Last Deglaciation Amsterdam, Netherlands Elsevier. pp. 571-579
AuthorsHughes, P.D., Allard, J., Woodward, J. and Pope, R.
EditorsPalacios, D., Hughes, P. D., García-Ruiz, J. M. and Andrés, N.
Abstract

The Younger Dryas Stadial is relatively muted in palaeoclimate records from the Balkans, especially in pollen records from lakes and bogs in the western Balkans where moisture supply did not fall markedly through this interval. There is, however, evidence of cooling and glacier expansion dated to the Younger Dryas in the southern and western Balkans. Strong west-east precipitation gradients are indicated by an increase in steppe taxa in pollen records. This is also reflected in marked rises in glacier equilibrium line altitudes (ELAs) from west to east.

KeywordsLate-glacial; cirque glaciers; Mediterranean; Late Pleistocene
Page range571-579
Year2022
Book title European Glacial Landscapes: The Last Deglaciation
PublisherElsevier
Place of publicationAmsterdam, Netherlands
ISBN9780323918992
Digital Object Identifier (DOI)https://doi.org/10.1016/B978-0-323-91899-2.00047-4
Web address (URL)https://www.sciencedirect.com/science/article/pii/B9780323918992000553
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File Access Level
Controlled
Output statusPublished
Publication dates
Online23 Sep 2022
Publication process dates
Deposited13 Feb 2023
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