Isle of Whithorn Dykes
Carghidown Formation-Wacke. These sedimentary rocks are marine in origin. They are detrital and comprise coarse- to fine-grained slurries of debris from the continental shelf flowing into a deep-sea environment, forming distinctively graded beds. Minimum Age (Years): 433,400,000 Minimum Period: Sil…
- Contributor
- dh1
- Location
- 54.69670, -4.36114
- Formation
- Carghidown Formation (Silurian)
- Licence
- License.ALL_RIGHTS_RESERVED
- Last updated
- 2026-05-14