What is recorded here
Clogwyn y Garnedd is a sea cliff composed primarily of Silurian greywacke and slate, formed around 440–420 million years ago through sedimentation and subsequent regional metamorphism. It is notable for its exposure of ancient volcanic and sedimentary rocks that are part of the Caledonian mountain-building event.
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Places near here
Yr WyddfaMountain / peak · 280 yd
Hafod Eryri Summit Visitor CentreVisitor information · 309 yd
Hafod Eryri, Rheilffordd Yr Wyddfa; Hafod Eryri, Snowdon Mountain Railway; Snowdon Summit Station; Snowdon Summit Railway TerminusCafe; Railway Station · 310 yd
Snowdon Summit StationHeritage place · 357 yd
Britannia MineMine · 921 yd
Garnedd UgainMountain / peak · 965 yd
Clogwyn DuCliff · 1374 yd
LliweddCliff · 1439 yd
Y Lliwedd (West Peak)Mountain / peak · 1517 yd
Rallt Goch - the red hillMountain or hill · 1520 yd
Llyn Llydaw Lake, Yr Wyddfa, Findspot of Wooden Boat or Dugout CanoeLake; Findspot · 1.0 mi
Cwm LlanWaterfall · 1.8 miOther information
Photo: Peter Holmes · CC BY-SA 2.0