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About: Dalradian     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Substance100019613, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:WikicatMetamorphicRocksyago:Abstraction100002137yago:Arrangement107938773yago:Formation108426461yago:Group100031264yago:Material114580897yago:Matter100020827yago:MetamorphicRock114698698yago:Part113809207yago:PhysicalEntity100001930yago:Relation100031921yago:WikicatGeologicFormationsOfTheUnitedKingdomyago:Rock114696793yago:Substance100019613 New Facet based on Instances of this Class

The Dalradian Supergroup (informally and traditionally the Dalradian) is a stratigraphic unit (a sequence of rock strata) in the lithostratigraphy of the Grampian Highlands of Scotland and in the north and west of Ireland. The diverse assemblage of rocks which constitute the supergroup extend across Scotland from Islay in the west to Fraserburgh in the east and are confined by the Great Glen Fault to the northwest and the Highland Boundary Fault to the southeast. Much of Shetland east of the Walls Boundary Fault is also formed from Dalradian rocks. Dalradian rocks extend across the north of Ireland from County Antrim in the north east to Clifden on the Atlantic coast, although obscured by later Palaeogene lavas and tuffs or Carboniferous rocks in large sections.