On deglaciation between Pieksämäki and Pielavesi in central Finland
On the basis of four end moraine formations, some of them not known before, the phases of deglaciation between Pieksämäki and Pielavesi in central Finland have been described in this paper. The trend of these end moraines, other transverse formations and radial eskers show that the ice retreated nor...
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| Format: | Article |
| Language: | English |
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Geological Society of Finland
1974-06-01
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| Series: | Bulletin of the Geological Society of Finland |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume46/sgs_bt_046_1_pages_043_051.pdf |