| Reference Type | Journal (article/letter/editorial) |
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| Title | On the origin of Grunty Fen and other landforms in southern Fenland, Cambridgeshire |
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| Journal | Geological Magazine |
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| Authors | West, R. G. | Author |
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| Year | 1991 (May) | Volume | 128 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s001675680002210xSearch in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 255036 | Long-form Identifier | mindat:1:5:255036:1 |
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| GUID | 0 |
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| Full Reference | West, R. G. (1991) On the origin of Grunty Fen and other landforms in southern Fenland, Cambridgeshire. Geological Magazine, 128 (3) 257-262 doi:10.1017/s001675680002210x |
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| Plain Text | West, R. G. (1991) On the origin of Grunty Fen and other landforms in southern Fenland, Cambridgeshire. Geological Magazine, 128 (3) 257-262 doi:10.1017/s001675680002210x |
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| In | (1991, May) Geological Magazine Vol. 128 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractDepressions and embayments of the southern Fenland margin and islands are ascribed to periglacial processes in the Devensian Stage (last cold stage) of the Pleistocene. The processes, which may be included in the general term thermokarst, include thermal erosion as an important element. The age of the active landscape evolution appears to be Late Devensian. The Crowland Bed of the Fenland Pleistocene succession is a product of these processes. |
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