| Reference Type | Journal (article/letter/editorial) |
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| Title | IV.—The Ice Age in England |
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| Journal | Geological Magazine |
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| Year | 1915 (November) | Series:Volume | 6:2 |
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| Issue | 11 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800203658 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 262885 | Long-form Identifier | mindat:1:5:262885:5 |
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| GUID | 0 |
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| Full Reference | (1915) IV.—The Ice Age in England. Geological Magazine, S. 6 Vol. 2 (11) 504-513 doi:10.1017/s0016756800203658 |
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| Plain Text | (1915) IV.—The Ice Age in England. Geological Magazine, S. 6 Vol. 2 (11) 504-513 doi:10.1017/s0016756800203658 |
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| In | (1915, November) Geological Magazine S. 6 Vol. 2 (11) Cambridge University Press (CUP) |
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| Abstract/Notes | In the preceding paragraphs it has been shown that, after the inland ice had attained its southernmost limit and had spent its force, there commenced in Southern England the last of many stages of land depression. This carried with it a complete reversal: the temperature was raised, the periphery of the inland ice melted, its pressure was lessened, and a rapid rise of the land—the Mousterian elevation—introduced a great rise, to which the origin of the submerged forests bears witness. Nevertheless, the greatest part of the land depression persisted even after Mousterian time, and this explains the continuance of the melting and its increased rapidity, as well as the rapid northward withdrawal of the inland ice, which we shall soon consider. |
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