From valley to marginal glaciation in alpine-type relief: Lateglacial glacier advances in the Pięć Stawów Polskich/Roztoka Valley, High Tatra Mountains, Poland
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- 作者：Jerzy Zasadnia ; jerzyzasadni@geol.agh.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Piotr Kłapytab ; woytastry@gmail.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Glacial geomorphology ; Schmidt hammer dating ; Lateglacial ; High Tatra Mountains
- 刊名：Geomorphology
- 出版年：2016
- 出版时间：15 January 2016
- 年：2016
- 卷：253
- 期：Complete
- 页码：406-424
- 全文大小：5107 K
文摘
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Mapping and Schmidt hammer (SH) datings in a key locality in the Tatra Mts
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5 Lateglacial stages, LGM, pre-B/A and YD surfaces discriminated in SH rebound test
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ELA rise over valley hypsometry maximum caused reorganization of deglaciation pattern.
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Likely no glaciers already in B/A; renewed YD advance — marginal type of glaciation
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Early-dry and later-wet YD climate revealed in geomorphic record.