Evolution of eolian relief of the Kaamasjoki–Kiellajoki river basin in Finnish Lapland
The aim of this study is to explain the dunes and deflation relief formed from sediments accumulated in an ice‑dammed lake during the deglaciation in the Kaamasjoki‑Kiellajoki river basin (69°15’‑69°25'N, 26°30'‑27°05'E). At present the dunes are parabolic fossil dunes formed in peri...
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Format: | Article |
Language: | English |
Published: |
Geographical Society of Finland
1971-01-01
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Series: | Fennia: International Journal of Geography |
Online Access: | https://fennia.journal.fi/article/view/40756 |