| Reference Type | Journal (article/letter/editorial) |
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| Title | IV.—Note on the Source of the Pebbles of the Bunter Pebble-beds of the English Midlands |
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| Journal | Geological Magazine |
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| Year | 1914 (May) | Series:Volume | 6:1 |
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| Page(s) | 211-215 | Issue | 5 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800196773 |
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| Mindat Ref. ID | 262295 | Long-form Identifier | mindat:1:5:262295:2 |
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| GUID | 893e8ac7-a853-4b7b-b615-8ef51e73fee1 |
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| Full Reference | (1914) IV.—Note on the Source of the Pebbles of the Bunter Pebble-beds of the English Midlands. Geological Magazine, S. 6 Vol. 1 (5) 211-215 doi:10.1017/s0016756800196773 |
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| Plain Text | (1914) IV.—Note on the Source of the Pebbles of the Bunter Pebble-beds of the English Midlands. Geological Magazine, S. 6 Vol. 1 (5) 211-215 doi:10.1017/s0016756800196773 |
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| In | (1914, May) Geological Magazine S. 6 Vol. 1 (5) Cambridge University Press (CUP) |
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| Abstract/Notes | The subject of the derivation of the materials which form the Bunter Pebble-beds has given rise to wide differences of opinion and to a voluminous literature. These it is not my intention to recapitulate, as an excellent summary of the subject will be found in Mr. O. H. Shrubsole's paper of 1903. Mr. Shrubsole then gathered together the known evidence, added some new facts of his own, and came to the conclusion that the Midland Bunter pebbles were brought from a southerly direction. This opinion may be said to have held the field until recently, when the question was again taken up by Mr. Jukes-Browne in the third edition of The Building of the British Isles (1911). After reviewing the whole evidence and taking into consideration the results of an investigation by Mr. E. C. Martin, which tended to show that the direction of transportation in Somersetshire in Bunter times was towards the south, Mr. Jukes-Browne abandoned the view he had taken in the second edition (1892) of that work, and now, adopting in the main the conclusions of Professor Bonney, considers that the bulk of the pebbles of the Midland Bunter came from the north-west, though he agrees that the fossiliferous quartzite pebbles could not have come from that direction, and he suggests for these a south-easterly derivation (Suffolk). |
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