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| Main Authors: | , , |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
1990
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.54300 |
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Table of Contents:
- A core from the deepest part of lake Königsegg. near Ostrach (Oberschwaben), has been studied palynologically and lithologically. The core is only 4.6 m long; lacustrine sedimentation began in the Oldest Dryas. The Alleroedian pumice tuff from Laacher See (Eifel) is present. The origin of the lake as a dead ice lake and its limnogeological development are briefly discussed.