| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | The Igneous Rocks of the Stanner-Hanter District, Radnorshire |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Holgate, Norman | Author |
|---|
| Knight Hallowes, K. A. | Author |
| Year | 1941 (August) | Volume | 78 |
|---|
| Issue | 4 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800071971 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 247204 | Long-form Identifier | mindat:1:5:247204:5 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Holgate, Norman, Knight Hallowes, K. A. (1941) The Igneous Rocks of the Stanner-Hanter District, Radnorshire. Geological Magazine, 78 (4) 241-267 doi:10.1017/s0016756800071971 |
|---|
| Plain Text | Holgate, Norman, Knight Hallowes, K. A. (1941) The Igneous Rocks of the Stanner-Hanter District, Radnorshire. Geological Magazine, 78 (4) 241-267 doi:10.1017/s0016756800071971 |
|---|
| In | (1941, August) Geological Magazine Vol. 78 (4) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | The igneous rocks of the Stanner-Hanter district are included within the Geological Survey I-inch map, sheet 56 S.E., (Old Series), and form three hog-backed hills, Stanner Rocks, Worsell Wood, and Hanter Hill, which are prominent features in the country between New Radnor and Kington, close to the Welsh border. This line of hills trends from south-west to north-east, though the separate ridges are arranged en échelon. Stanner Rocks (I,08I feet), is separated from Worsell Wrood (about 940 feet), by the alluvial plain of the Gilwern Brook, while there is a low col between Worsell Wood and Hanter Hill (I,36I feet). |
|---|
These are possibly similar items as determined by title/reference text matching only.
