
What is recorded here
Falcon Clints is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The feature is notable for its well-exposed clint and gully structures, which result from differential erosion and provide insight into the region's geological history.
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Places near here
Waterfall in TeesdaleWaterfall · 398 yd
Lower Falls at Cauldron SnoutWaterfall · 973 yd
Cauldron Snout (Waterfall)Viewpoint · 978 yd
Fox EarthsCliff · 1546 yd
Cronkley ScarCliff · 1.7 mi
Cow Green ReservoirHeritage attraction · 1.8 mi
Touting HillMountain / peak · 2.2 mi
Haugh HillMountain / peak · 2.5 mi
Langdon Beck PlantationWood · 2.6 mi
Old Milestone by the B6277, GreenhillsMonument or public art · 2.6 mi
Milestone at Hanging ShawListed building · 2.9 mi
Meldon HallRuins · 2.9 miOther information
Photo: Mick Garratt · CC BY-SA 2.0