| Reference Type | Journal (article/letter/editorial) |
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| Title | II.—The Uppermost Silurian and Old Red Sandstone of South Staffordshire |
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| Journal | Geological Magazine |
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| Year | 1912 (November) | Series:Volume | 5:9 |
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| Issue | 11 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800115845 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 276366 | Long-form Identifier | mindat:1:5:276366:2 |
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|
| GUID | 0 |
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| Full Reference | (1912) II.—The Uppermost Silurian and Old Red Sandstone of South Staffordshire. Geological Magazine, S. 5 Vol. 9 (11) 484-491 doi:10.1017/s0016756800115845 |
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| Plain Text | (1912) II.—The Uppermost Silurian and Old Red Sandstone of South Staffordshire. Geological Magazine, S. 5 Vol. 9 (11) 484-491 doi:10.1017/s0016756800115845 |
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| In | (1912, November) Geological Magazine S. 5 Vol. 9 (11) Cambridge University Press (CUP) |
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| Abstract/Notes | 2. The Downton Castle or Yellow Sandstones (see Figs. 2 and 3).— These occur at Lye and Turners Hill, but the best sections are at Saltwells. There the lowest beds are 10 feet of brown yellow and blue soft sandy mudstones (see Fig. 2, Ea), seen resting on the Ludlow Bone-bed, north of the Tram Bridge. Like the same zone at Ludlow, they are practically unfossiliferous. |
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These are possibly similar items as determined by title/reference text matching only.
