| Reference Type | Journal (article/letter/editorial) |
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| Title | V.—On Some Points in Anglesey Geology |
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| Journal | Geological Magazine |
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| Year | 1882 (August) | Series:Volume | 2:9 |
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| Issue | 8 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800171523 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 277587 | Long-form Identifier | mindat:1:5:277587:0 |
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| GUID | 0 |
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| Full Reference | (1882) V.—On Some Points in Anglesey Geology. Geological Magazine, S. 2 Vol. 9 (8) 362-363 doi:10.1017/s0016756800171523 |
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| Plain Text | (1882) V.—On Some Points in Anglesey Geology. Geological Magazine, S. 2 Vol. 9 (8) 362-363 doi:10.1017/s0016756800171523 |
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| In | (1882, August) Geological Magazine S. 2 Vol. 9 (8) Cambridge University Press (CUP) |
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| Abstract/Notes | In my former short communication on this subject, I referred only to the question of the age of the quartz conglomerate at Nebo, which Dr. Callaway mistook for a part of the granitoidite series, but which Prof. Hughes has shown to be Cambrian conglomerate. What Dr. Callaway says in reply may be seen at page 287. The second point which I stated I should deal with later, I now take up. Dr. Callaway wrote (GEOL. MAG. 1881, p. 423), as follows :— |
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These are possibly similar items as determined by title/reference text matching only.
