The Bowmore Sandstone Group is a sequence of metasedimentary rocks, dominantly sandstones, of probable Neoproterozoic age. Their outcrop on the island of Islay in the Inner Hebrides is entirely fault-bounded, between the Loch Gruinart Fault to the west and the Loch Skerrols Shear Zone to the east.[1]
References
- ^ McAteer C.A.; Daly J.S.; Flowerdew M.J. & Whitehouse M.J. (2010). "Dalradian Grampian Group affinity for the Bowmore Sandstone Group, Islay". Scottish Journal of Geology. 46: 97–111. doi:10.1144/0036-9276/01-408. S2CID 140565408.
| Villages |  | |
|---|---|---|
| Geographical features | ||
| History and architecture |
| |
| Islay whisky | ||
| Other Islay related articles | ||
You must be logged in to post a comment.