Cregennen Formation

Geologic formation in Wales From Wikipedia, the free encyclopedia

The Cregennen Formation is a geological formation of early Darriwilian age (late Middle Ordovician). It consists of dark grey to black mudstones containing graptolites, with interbedded volcanic units, particularly felsic and mafic tuffs.[1]

Sub-unitsCefn Hir Member, Bryn Brith Member
UnderliesBrithion Formation, Llyn y Gafr Volcanic Formation
Quick facts Type, Unit of ...
Cregennen Formation

Stratigraphic range: Darriwilian
Acidic tuffs of the Cefn Hir Member near the summit of Pared-y-Cefn Hir, Gwynedd, Wales
TypeGeological formation
Unit ofAran Volcanic Group
Sub-unitsCefn Hir Member, Bryn Brith Member
UnderliesBrithion Formation, Llyn y Gafr Volcanic Formation
OverliesOffrwm Volcanic Formation
Thicknessup to 350 metres (1,150 ft)
Location
CountryWales
Type section
Named forLlynnau Cregennen
Close
Prominent ridges of Pared y Cefn-Hir (to the right) and Bryn Brith (to the left) viewed from the southwest, formed of volcanic members of the Cregennen Formation

Two larger volcanic units developed are the Cefn Hir and Bryn Brith members that form the prominent ridges of Pared-y-Cefn-Hir and Bryn Brith.[2][3]

References

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