Late Glacial and Holocene paleoenvironmental records in the Tatra Mountains, East-Central Europe, based on lake, peat bog and colluvial sedimentary data: A summary review

The Tatra Mountains are the highest massif in the Carpathian mountain arc (2655 m) and represent a typical alpine landscape developed in the course of Pleistocene glaciations, but are not glacierized today. The glacial relief of the massif offers an abundance of topographic depressions (cirque overd...

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Bibliographic Details

Published in:	Quaternary international Vol. 415; pp. 126 - 144
Main Authors:	Kłapyta, Piotr, Zasadni, Jerzy, Pociask-Karteczka, Joanna, Gajda, Agnieszka, Franczak, Paweł
Format:	Journal Article
Language:	English
Published:	Elsevier Ltd 10-09-2016
Subjects:	Holocene Lake sediments Late Glacial Little Ice Age Peat bogs Tatra Mountains Peat bogs Tatra Mountains Lake sediments Little Ice Age Holocene Late Glacial
Online Access:	Get full text
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