| Loch Ness Supergroup | |
|---|---|
| Stratigraphic range: 900–850 Ma | |
 Vertically banded rocks of the Glenfinnan Group | |
| Type | Geological supergroup |
| Sub-units | Loch Eil Group, Glenfinnan Group, Badenoch Group |
| Underlies | Dalradian Supergroup |
| Overlies | Wester Ross Supergroup with tectonic contact |
| Area | Northwestern Scotland |
| Thickness | 6–9 km |
| Lithology | |
| Primary | Semi-pelite, Pelite, Psammite |
| Other | Quartzite |
| Type section | |
| Named for | Loch Ness |
The Loch Ness Supergroup is one of the subdivisions of the Neoproterozoic sequence of sedimentary rocks (or their metamorphic equivalents) in the Scottish Highlands.[1] It is found everywhere in tectonic contact above the older Wester Ross Supergroup. It is thought to be unconformably overlain by the Cryogenian to Cambrian Dalradian Supergroup.[2]
- ^ British Geological Survey. "Loch Ness Supergroup". BGS Lexicon of named rock units. Retrieved 31 May 2024.
- ^ Krabbendam, M.; Strachan, R.; Prave, T. (2022). "A new stratigraphic framework for the early Neoproterozoic successions of Scotland". Journal of the Geological Society. 179. doi:10.1144/jgs2021-054. hdl:10023/24155.