Llewelyn Volcanic Group
Stratigraphic range: Caradoc Ordovician
Rhyolitic ash-flow tuffs of the Capel Curig Volcanic Formation exposed on the northeastern face of Pen yr Ole Wen, capped by sandstones of the overlying Cwm Eigiau Formation, which can be seen at the top of the face
Type	Group
Sub-units	Capel Curig Volcanic Formation, Foel Fras Volcanic Formation, Conwy Rhyolite Volcanic Formation, Foel Grach Basalt Formation, Braich Tu Du Volcanic Formation
Underlies	Cwm Eigiau Formation
Overlies	Nant Ffrancon Formation
Thickness	approx 1400m
Lithology
Primary	ash flow tuffs
Other	rhyolites, mudstones, siltstones, sandstones, breccias etc
Location
Region	northwest Wales
Country	Wales
Type section
Named for	Carnedd Llewelyn

The Llewelyn Volcanic Group is an Ordovician lithostratigraphic group (a sequence of rock strata) in Snowdonia, north-west Wales. The name is derived from Carnedd Llewelyn, the highest peak in the Carneddau range where it outcrops.

Outcrops

The rocks occur across the Snowdon massif and the Carneddau and within the Capel Curig Anticline.^[1]

Lithology and stratigraphy

The Group comprises around 1400m thickness of ash flow tuffs, flow-banded rhyolites and breccias with a variety of volcaniclastic sediments erupted or sedimented during the Caradocian epoch of the Ordovician period. The Group comprises (in descending order, i.e. oldest last):

• Capel Curig Volcanic Formation
• Foel Fras Volcanic Formation
• Conwy Rhyolite Volcanic Formation

It also includes the Foel Grach Basalt Formation and the Braich Tu Du Volcanic Formation.^[2]

References