A buried valley system in the Strait of Dover
A series of buried valleys situated south of the submerged Chalk outcrop of the Strait of Dover and eroded down to — 170 m n .g.f. || are recognized as infilled tunnel-valleys excavated subglacially during the Warthe Phase of the Saalian glaciation beneath an ice sheet that advanced up the English C...
| Published in: | Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
The Royal Society
1975
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1098/rsta.1975.0056 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1975.0056 |