Durness Group
The Durness Group is a geological group, a stratigraphic unit, formed mainly of dolomites of late Cambrian to early Ordovician age.[1] It outcrops along the full strike extent of the Moine Thrust Belt in the Northwest Highlands of Scotland. Within the thrust belt it is often affected by thrust faulting.
Durness Group Stratigraphic range: Cambrian–Ordovician | |
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Dolomites of the Durness Group with schists of the Moine Supergroup thrust over them on the Moine Thrust at Knockan Crag | |
Type | Group |
Sub-units | Ghrudaidh Formation, Eilean Dubh Formation, Sailmhor Formation, Sangomore Formation, Balnakiel Formation, Croisaphuill Formation, Durine Formation |
Underlies | Moine Supergroup along the Moine Thrust. |
Overlies | An t-Sron Formation of the Ardvreck Group |
Thickness | up to 750 m (2,460 ft) |
Lithology | |
Primary | Dolomite |
Other | Limestone, chert |
Location | |
Region | Northwest Highlands |
Country | |
Type section | |
Named for | Durness |
References
- "Durness Group". BGS Lexicon of Named Rock Units. British Geological Survey. Retrieved 30 July 2018.
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