What is recorded here
Chambers Crag is a sea cliff composed of Carboniferous limestone, formed approximately 340 to 300 million years ago through the accumulation of marine sediments. It is notable for its exposure of durable limestone strata, which are significant for understanding the geological history of the Cumberland region.
This does not grant access. Check current paths, opening conditions and ownership before entering.
Places near here
Scafell PikeMountain / peak · 185 yd
Broad CragMountain / peak · 356 yd
Ill CragMountain / peak · 677 yd
Broad StandCliff · 921 yd
Dow CragCliff · 960 yd_-_geograph.org.uk_-_2610324.jpg?width=1280)
Cam Spout (upper waterfall)Waterfall · 1401 yd_-_geograph.org.uk_-_2610328.jpg?width=1280)
Cam Spout (waterfall)Waterfall · 1431 yd
Church of St OlafListed building · 2.0 mi
Monument at Wasdale Head Village GreenMonument or public art · 2.0 mi_Post_Box_(1837-1901),_Wasdale_Head_-_geograph.org.uk_-_7298519.jpg?width=1280)
Queen Victoria (VR) Post Box (1837-1901), Wasdale HeadOld post box · 2.1 mi
Fence WoodWood · 2.2 mi
Maiden Castle round cairn, BurnmoorScheduled monument · 2.3 mi