On the influence of latitudinal climatic zonation on the degradation of the Late Valday (Late Visla) glaciation with the example of marginal formations of the territories of Finland and Karelian-Kola region
It is established that the Keyva-2 ridge developed in the eastern Kola Peninsula is not a marginal formation of the Ponoy ice shield. It was mainly formed between the Kola and Belomorian glacial lobes of the late Valdai glaciation spread eastward. Using the example of the last cover glaciation, it h...
| Published in: | Vestnik MGTU |
|---|---|
| Main Author: | |
| Format: | Book |
| Language: | Russian |
| Published: |
2018
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| Subjects: | |
| Online Access: | http://hdl.handle.net/1834/17289 https://doi.org/10.21443/1560-9278-2018-21-1-18-25 |