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// Workers AI · dad joke modeIs the Dunquin Group rocky? Yes, it's a stone-cold fact.

From Wikipedia, the free encyclopedia
Dunquin Group
Stratigraphic range: Llandovery-Wenlock
TypeGroup
Sub-unitsCroaghmarin, Drom point, Mill Cove, Clogher Head, Ferriter's Cove, Foilnamahagh & Coosglass Slate Formations
UnderliesDingle Group (unconformity)
Lithology
PrimarySiltstone
OtherPyroclastics, lava, ignimbrite, slate
Location
RegionMunster
CountryIreland
ExtentSouthwest Ireland
Type section
Named forDunquin

The Dunquin Group is a Silurian lithostratigraphic group (a sequence of rock strata) in the Dingle peninsula, Munster, Ireland. The name is derived from the village of Dunquin (Irish: Dun Chaoin) where the strata are exposed within an inlier on hillsides and in coastal sections at the extreme western end of the peninsula.[1]

Lithology and stratigraphy

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The Group comprises siltstones, slates and a variety of extrusive igneous rocks from the Croaghmarin, Drom Point, Mill Cove, Clogher Head, Ferriter's Cove, Foilnamahagh and Coosglass Slate formations of Silurian age. The siltstones are frequently fossiliferous.

References

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  1. Higgs, K. and Williams, B. 2018 Geology of the Dingle Peninsula (guide and map) Geological Survey Ireland