Crackington Haven ( kw, Porthkragen, meaning "sandstone cove") is a coastal village in Cornwall, England, United Kingdom. It is in the civil parish of St Gennys at at the head of a cove on the Atlantic coast. The village is seven miles (11 km) south-southwest of Bude and four miles (7 km) north-northeast of Boscastle.Ordnance Survey: Landranger map sheet 190 ''Bude & Clovelly'' Middle Crackington and Higher Crackington are associated settlements. They are situated on the hill southeast of Crackington Haven, half-a-mile and one mile distant respectively.

Geography

Crackington Haven is popular with tourists, walkers and geology students. The surrounding cliffs are well known for their visible folded sedimentary rock formations. The village gives its name to the Crackington formation, a sequence of

Carboniferous The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carbonifero ...

sandstones and grey

shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especial ...

s. The village has two café-style tea rooms, and a pub called the Coombe Barton Inn in a building which was originally the house of the manager of a local slate quarry. Crackington Haven has a stony foreshore but a sandy beach is revealed at low water. The local parish council has put up signs asking that people do not remove stones, and saying that people who do will be prosecuted under the 1949 Coastal Protection Act. There are toilet facilities near the beach and lifeguard cover in the summer. Immediately north of the beach is Pencarrow Point and a few hundred yards south is Cambeak headland (between Tremoutha Haven and Cam Strand); the clifftop here is 328 ft. Cambeak is derived from Old Cornish and means "crooked point". One mile south of Crackington Haven, High Cliff rises to . It is Cornwall's highest cliff, (Great Hangman in Devon has a cliff face of . Crackington Haven lies within the Cornwall Area of Outstanding Natural Beauty (AONB). Almost a third of Cornwall has AONB designation, with the same status and protection as a National Park.

History

The manor of Crackington was recorded in the Domesday Book (1086) when it was one of several manors held by Berner from

Robert, Count of Mortain Robert, Count of Mortain, 2nd Earl of Cornwall (–) was a Norman nobleman and the half-brother (on their mother's side) of King William the Conqueror. He was one of the very few proven companions of William the Conqueror at the Battle of Hastin ...

. There was half a hide of land and land for 3 ploughs. There were 1 plough, 2 serfs, 6 smallholders, 4 acres of underwood, 20 acres of pasture, 4 cattle, 3 pigs and 25 sheep. The value of the manor was 10 shillings though it had formerly been worth £1 sterling.Thorn, C. et al., ed. (1979) ''Cornwall''. Chichester: Phillimore; entry 5,8,6 Until the nineteenth century, Crackington Haven was a small port similar to many others on the north coast of Cornwall. Limestone and coal were imported and slate and other local produce were exported. After the railways reached the district in 1893 the village could be reached more easily (from the North Cornwall Railway station at Otterham) so holidaymaking became more common. Crackington Haven was badly affected by the 2004 flood that damaged several other villages, notably Boscastle. The road bridge across the stream, several homes and the pub were damaged by floodwater.

References

{{authority control Beaches of Cornwall Villages in Cornwall Populated coastal places in Cornwall