Bowmore Sandstone Group
Bowmore Sandstone Group Stratigraphic range: Neoproterozoic | |
---|---|
Laggan Formation at Eilean Mhic Ghoile, near Bowmore, Islay | |
Type | Group |
Sub-units | Laggan Formation, Blackrock Formation |
Lithology | |
Primary | Sandstone |
Other | Shale, siltstone |
Location | |
Region | Inner Hebrides |
Type section | |
Named for | Bowmore |
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" (PDF). Scottish Journal of Geology 46: 97–111. doi:10.1144/0036-9276/01-408.
This article is issued from Wikipedia - version of the Saturday, June 20, 2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.