The glacial geomorphology of part of the Western Grampians of Scotland, with especial reference to the limits of the Loch Lomond Advance
The limits of a large ice mass that built up in the western Grampians during the Loch Lomond Stadial were mapped using O.S. maps to scales of 1 : 10,000 and 1 : 25,000. The main forms of mapped glacial evidence comprised moraines, thick till, fluvioglacial landforms, erratics, boulder spreads, ice-m...
| Үндсэн зохиолч: | |
|---|---|
| Формат: | Дипломын ажил |
| Хэл сонгох: | English |
| Хэвлэсэн: |
1984
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| Нөхцлүүд: | |
| Онлайн хандалт: | https://repository.londonmet.ac.uk/7669/1/349045.pdf |