| Reference Type | Journal (article/letter/editorial) |
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| Title | A Foraminiferous Clay at Bredwardine, Herefordshire |
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| Journal | Geological Magazine |
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| Authors | Grindley, H. E. | Author |
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| Year | 1923 (February) | Volume | 60 |
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| Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800084612 |
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| Generate Citation Formats |
| Mindat Ref. ID | 280411 | Long-form Identifier | mindat:1:5:280411:2 |
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| GUID | 0 |
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| Full Reference | Grindley, H. E. (1923) A Foraminiferous Clay at Bredwardine, Herefordshire. Geological Magazine, 60 (2) 88-90 doi:10.1017/s0016756800084612 |
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| Plain Text | Grindley, H. E. (1923) A Foraminiferous Clay at Bredwardine, Herefordshire. Geological Magazine, 60 (2) 88-90 doi:10.1017/s0016756800084612 |
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| In | (1923, February) Geological Magazine Vol. 60 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | Half a mile above Bredwardine Bridge on the Wye, 11½ miles above Hereford, the river on the right bank runs at the foot of an exposure of drift about 50 feet high, showing the following section: Clayey red sand with sandstone pebbles, subangular; lower 10 feet, more clayey with limestone and claystone pebbles, striated. |
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