| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Note on the Relation of the Upper and Lower Old Red Sandstone of Gower |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Williams, Daisy M. | Author |
|---|
| Year | 1926 (May) | Volume | 63 |
|---|
| Issue | 5 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800084144 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 280969 | Long-form Identifier | mindat:1:5:280969:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Williams, Daisy M. (1926) Note on the Relation of the Upper and Lower Old Red Sandstone of Gower. Geological Magazine, 63 (5) 219-223 doi:10.1017/s0016756800084144 |
|---|
| Plain Text | Williams, Daisy M. (1926) Note on the Relation of the Upper and Lower Old Red Sandstone of Gower. Geological Magazine, 63 (5) 219-223 doi:10.1017/s0016756800084144 |
|---|
| In | (1926, May) Geological Magazine Vol. 63 (5) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | The Old Red Sandstone occurs in Gower in several inliers which form hills rising above the undulating plateau of Carboniferous Limestone. The chief are Cefn-y-bryn (548 feet) in mid-Gower, Llanmadog Hill (609 feet), the westerly extension of Cefn-y-bryn in north-west Gower, and Rhosilli Down (633 feet) in the extreme west of Gower. |
|---|
These are possibly similar items as determined by title/reference text matching only.
