What is recorded here
Greenhow Crags is a sea cliff or coastal rock feature composed of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of sedimentary rock layers that provide insight into the geological history of the Cumberland region.
This does not grant access. Check current paths, opening conditions and ownership before entering.
Places near here
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Middle HowMountain / peak · 319 yd
UllscarfMountain / peak · 1107 yd
A waterfallWaterfall · 1365 yd
Waterfall on Wyth BurnWaterfall · 1482 yd
Broadstone HeadCliff · 1556 yd
Ash CragsCliff · 1615 yd
Old Milepost by the A591, Wythburn, Dunmail Raise ParishMonument or public art · 2.1 mi
Milestone, Dunmail RaiseMonument or public art · 2.2 mi
Wythburn ChurchListed building · 2.4 mi
Stake PassHeritage attraction · 2.4 mi
The CottageListed building · 2.5 mi
Greenhowe Caravan ParkWood · 2.8 mi