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 |
|---|---|
| Pages (from-to) | 333-351 |
| Number of pages | 19 |
| Journal | American Society of Mechanical Engineers (Paper) |
| Publication status | Published - 1986 |