Abstract
The uncertainty about the magnitude of the Vestfold glaciation during the terminal Pleistocene is stressed. Water and salt are seen as the major current geomorphological agents in the Hills. -P.J.Jarvis
Original language | English |
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Pages (from-to) | 333-351 |
Number of pages | 19 |
Journal | American Society of Mechanical Engineers (Paper) |
Publication status | Published - 1986 |