| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Structural Study of the Contorted Drift and Disturbed Chalk at Weybourne, North Norfolk. |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Banham, P. H. | Author |
|---|
| Ranson, C. E. | Author |
| Year | 1965 (April) | Volume | 102 |
|---|
| Issue | 2 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800057484Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 249491 | Long-form Identifier | mindat:1:5:249491:7 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Banham, P. H., Ranson, C. E. (1965) Structural Study of the Contorted Drift and Disturbed Chalk at Weybourne, North Norfolk. Geological Magazine, 102 (2) 164-174 doi:10.1017/s0016756800057484 |
|---|
| Plain Text | Banham, P. H., Ranson, C. E. (1965) Structural Study of the Contorted Drift and Disturbed Chalk at Weybourne, North Norfolk. Geological Magazine, 102 (2) 164-174 doi:10.1017/s0016756800057484 |
|---|
| In | (1965, April) Geological Magazine Vol. 102 (2) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractA structural analysis of the cliffs and one pit section in Pleistocene deposits at Weybourne has shown one major phase of ice movement only. Ice moving from approximately 210 degrees caused the disturbance of the upper part of the Chalk (together with the overlying Weybourne Crag) and the deformation and deposition of a chalky-boulder-clay, thought to be equivalent to the Lowestoft till. |
|---|
These are possibly similar items as determined by title/reference text matching only.
