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Summary
| Description |
English: (a) Simplified geological map showing the area between Old Radnor and Presteigne and the coeval succession of the Malvern Hills. Note that the red dashed lines highlight the approximate trends of the Church Stretton Fault Zone (CSFZ) and Malvern Line (ML). Contains British Geological Survey materials © UKRI (2021). (b) The age and thickness of the succession encountered within the study area, based upon the results of the study herein. Early (e), middle (m), and late (l) subdivisions have been given for the stages, as have the internationally recognized stage slices. (c) Palaeogeographic context of the Old Radnor and Presteigne study area during middle Sheinwoodian times; estimated palaeolatitude of study area 13°S of the equator [31, 94]. CSFZ = Church Stretton Fault Zone; MH = Malvern Hills; ML = Malvern Line; Pem. = Pembrokeshire. (d) The location in details. |
| Date | |
| Source | The Silurian Transgression of a Palaeoshoreline: The Area between Old Radnor and Presteigne, Welsh Borderlands. Lithosphere. 2021 (1): 7866176. (2021) doi:10.2113/2021/7866176 |
| Author | David C. Ray; Emilia Jarochowska; Helen E. Hughes; Anna L. Claussen; Arthur C. Tingley; John Moseley; Oskar Bremer |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 10:14, 16 January 2022 | | 986 × 1,403 (672 KB) | Chhandama | Uploaded a work by David C. Ray; Emilia Jarochowska; Helen E. Hughes; Anna L. Claussen; Arthur C. Tingley; John Moseley; Oskar Bremer from The Silurian Transgression of a Palaeoshoreline: The Area between Old Radnor and Presteigne, Welsh Borderlands. Lithosphere. 2021 (1): 7866176. (2021) doi:10.2113/2021/7866176 with UploadWizard |
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