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Crackington Haven (, 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 south-southwest of Bude and 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 sandstones and grey shales. The village has two café-style tea rooms, and a pub called the Coombe Barton Inn in a building that was originally the house of a local slate quarry manager. Crackington Haven has a sto ...
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Crackington Haven
Crackington Haven (, 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 south-southwest of Bude and 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 sandstones and grey shales. The village has two café-style tea rooms, and a pub called the Coombe Barton Inn in a building that was originally the house of a local slate quarry manager. Crackington Haven has a s ...
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St Gennys
St Gennys () is a coastal civil parish and small settlement in north Cornwall, England, United Kingdom. The village of St Gennys is about southwest of Bude.Ordnance Survey: Landranger map sheet 190 ''Bude & Clovelly'' It is on high ground half-a-mile north of the coastal village of Crackington Haven, the major settlement in the parish. The only other settlements of any size in the parish are Middle Crackington and Higher Crackington both of which are southeast of Crackington Haven, half-a-mile and one mile distant respectively. The population of the parish at the 2011 census was 873. History and geography The name St Gennys is generally thought to derive from 4th Century Christian martyr Saint Genesius although it has been suggested that the commemoration is to the Welsh Saint Gwynws. In either case the name is old and several places in the parish are mentioned in the Domesday Book including Crackington (as ''Crachemua''), Dizzard (as ''Disart'') and St Gennys itself (as ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers (Lamination (geology), laminae) less than one centimeter in thickness. This property is called ''Fissility (geology), fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the narrower sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks in ...
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Beaches Of Cornwall
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rap ...
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Boscastle Flood Of 2004
The 2004 Boscastle flood occurred on Monday 16 August 2004 in the two villages of Boscastle and Crackington Haven in Cornwall, England, United Kingdom. The villages suffered extensive damage after flash floods caused by an exceptional amount of rain that fell over eight hours that afternoon. The flood in Boscastle was filmed and extensively reported, but the floods in Crackington Haven and Rocky Valley were not mentioned beyond the local news. The floods were the worst in local memory. A study commissioned by the Environment Agency from hydraulics consulting firm HR Wallingford concluded that it was among the most extreme ever experienced in Britain. The peak flow was about 140 m3/s, between 5:00 pm and 6:00 pm BST. The annual chance of this (or a greater) flood in any one year is about 1 in 400. The probability each year of the heaviest three-hour rainfall is about 1 in 1300 (although rainfall probability is not the same as flood probability). At midday on 16 Augu ...
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Otterham
Otterham () is a village and a civil parish in north Cornwall, England, United Kingdom. The village is situated approximately south of Bude and north of Camelford.Ordnance Survey: Landranger map sheet 190 ''Bude & Clovelly'' Otterham Mill, Otterham Down and Otterham Station (''see below'') are neighbouring settlements to Otterham village; all take the name from the River Ottery which rises in the parish. The parish is in the Hundred of Lesnewth and Deanery of Trigg Major. It is in the Registration District of Camelford and belongs to the Boscastle group of Anglican parishes. Otterham parish is bounded to the north by St Gennys, to the east by Warbstow, to the south by Davidstow and to the west by St Juliot. The parish is rural with small hamlets and farmsteads spread fairly evenly across it: the population of the parish in the 2001 census was 228. The parish church of St Denis at is in Otterham village and has a 40 ft tower housing three bells. The church was estab ...
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North Cornwall Railway
The North Cornwall Railway (NCR) also known as the North Cornwall Line, was a standard gauge railway line running from Halwill in Devon, to Padstow in Cornwall, at a distance of via Launceston, Camelford and Wadebridge. The line was opened in late 19th century by the North Cornwall Railway Company with support throughout much of its construction and existence by the London and South Western Railway (LSWR). The railway line was part of a drive by the LSWR to expand its influence in the South West, connect its rail network with the Bodmin and Wadebridge line, and to develop both holiday and freight traffic to Cornwall. The LSWR had opened a line connecting Exeter with Holsworthy in 1879, and by encouraging the NCR it planned to create railway access to previously inaccessible parts of the northern coastal area. As part of the 1923 railway groupings, the North Cornwall line came under the full ownership of LSWR, as the LSWR itself came under the ownership of Southern Railw ...
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Robert, Count Of Mortain
Robert, Count of Mortain, first Earl of Cornwall of 2nd creation (–) 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 Hastings and as recorded in the Domesday Book of 1086 was one of the greatest landholders in his half-brother's new Kingdom of England. Life Robert was the son of Herluin de Conteville and Herleva of Falaise and brother of Odo of Bayeux.Detlev Schwennicke, ''Europäische Stammtafeln: Stammtafeln zur Geschichte der Europäischen Staaten'', Neue Folge, Band III Teilband 4 (Marburg, Germany: Verlag von J. A. Stargardt, 1989), Tafel 694B Robert was born in Normandy, a half-brother of William the Conqueror. and was probably not more than a year or so younger than his brother Odo, born . About 1035, Herluin, as Vicomte of Conteville, along with his wife Herleva and Robert, founded Grestain Abbey. Count of Mortain Around 1049 ...
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Domesday Book
Domesday Book ( ; the Middle English spelling of "Doomsday Book") is a manuscript record of the Great Survey of much of England and parts of Wales completed in 1086 at the behest of William the Conqueror. The manuscript was originally known by the Latin name , meaning "Book of Winchester, Hampshire, Winchester", where it was originally kept in the royal treasury. The ''Anglo-Saxon Chronicle'' states that in 1085 the king sent his agents to survey every shire in England, to list his holdings and dues owed to him. Written in Medieval Latin, it was Scribal abbreviation, highly abbreviated and included some vernacular native terms without Latin equivalents. The survey's main purpose was to record the annual value of every piece of landed property to its lord, and the resources in land, labour force, and livestock from which the value derived. The name "Domesday Book" came into use in the 12th century. Richard FitzNeal wrote in the ( 1179) that the book was so called because its de ...
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Cornwall Area Of Outstanding Natural Beauty
The Cornwall National Landscape (formerly the Cornwall Area of Outstanding Natural Beauty) covers in Cornwall, England, United Kingdom; that is, about 27% of the total area of the county. It comprises 12 separate areas, designated under the National Parks and Access to the Countryside Act 1949 for special landscape protection. Of the areas, eleven cover stretches of coastline; the twelfth is Bodmin Moor. The areas are together treated as a single Area of Outstanding Natural Beauty (AONB): all AONBs have been rebranded as National Landscapes since November 2023. Section 85 of the Countryside and Rights of Way Act 2000 places a duty on all relevant authorities when discharging any function affecting land within an AONB to have regard to the purpose of conserving and enhancing natural beauty. Section 89 places a statutory duty on Local Planning Authorities with an AONB within their administrative area to produce a 5-year management plan. Designation The areas were designated in ...
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Weatherhill, Craig
Craig Weatherhill (1950 or 1951 – 18 or 19 July 2020) was a Cornish antiquarian, novelist and writer on the history, archaeology, place names and mythology of Cornwall. Weatherhill attended school in Falmouth, where his parents ran a sports shop. He played football for a number of local clubs, including Mawnan, and played as goalkeeper for the county football team. Between 1972 and 1974, Weatherhill served with the RAF, training as a cartographer. He was discharged after a serious back injury. He worked as a planning officer, architectural designer and historic conservation expert in local government and private practice. Under the tutelage of historian P.A.S. Pool he conducted archaeological surveys of West Cornwall. Weatherhill was also a Conservation Officer at Penwith District Council. He contributed to the BBC's Radyo Kernow, in particular to the series ''The Tinners' Way'' and ''Beachcombers''. In 1981 Weatherhill was made a Bard of Gorsedh Kernow for services to Co ...
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Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ...
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