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Trebetherick
Trebetherick ( kw, Trebedrek) is a village on the north coast of Cornwall. It is situated on the east side of the River Camel estuary approximately six miles (10 km) north of Wadebridge and half a mile (800 metres) south of Polzeath.Ordnance Survey: Landranger map sheet 200 ''Newquay & Bodmin'' Trebetherick straddles the Polzeath to Wadebridge road and extends west to Daymer Bay and northwest to Trebetherick Point, a rocky headland in the estuary, where the remains of shipwrecks can be seen on the foreshore. The National Trust owns land adjacent to Trebetherick Point. Geography South of Trebetherick Point is Daymer Bay with a sandy beach sheltered from the Atlantic. The beach provides safe bathing for holidaying families and is also popular with windsurfers. At the south end of Daymer Bay Brea Hill rises to 62 metres (203 feet) with several tumuli at the summit. Behind Daymer Bay's sand dunes and south of Trebetherick is the St Enodoc Golf Club's golf course. Between i ...
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River Camel
The River Camel ( kw, Dowr Kammel, meaning ''crooked river'') is a river in Cornwall, England. It rises on the edge of Bodmin Moor and with its tributaries its catchment area covers much of North Cornwall. The river flows into the eastern Celtic Sea between Stepper Point and Pentire Point having covered about 30 miles, making it the second longest river wholly in Cornwall. The river is tidal upstream to Egloshayle and is popular for sailing, birdwatching and fishing. The name ''Camel'' comes from the Cornish language for 'the crooked one', a reference to its winding course. Historically the river was divided into three named stretches. Heyl ( kw, Heyl, meaning ''estuary'') was the name for the estuary up to Egloshayle, the River Allen ( kw, Dowr Alen, meaning ''shining river'') was the stretch between Egloshayle and Trecarne, whilst the Camel was reserved for the stretch of river between its source and Trecarne. Geology and hydrology The River Camel rises on Hendraburnick Do ...
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St Enodoc's Church, Trebetherick
St. Enodoc Church, Trebetherick (Old kw, Gwenedek, ''St. Guenedoc'') is a chapel in the parish of St Minver. It is located to the south of the village of Trebetherick, Cornwall, England, United Kingdom (). It is a Grade I listed building. Background The church is situated in sand dunes east of Daymer Bay and Brea Hill on the River Camel estuary. Wind-driven sand has formed banks that are almost level with the roof on two sides. From the sixteenth century to the middle of the nineteenth century, the church was virtually buried by the dunes and was known locally as "Sinking Neddy" or "Sinkininny Church". To maintain the tithes required by the church, it had to host services at least once a year, so the vicar and parishioners descended into the sanctuary through a hole in the roof (see Talk). By 1864 it was unearthed and the dunes were stabilized. The church is surrounded by the Church course of the St Enodoc Golf Club. History The church is said to lie on the site of a cave where ...
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Brea Hill, Trebetherick
Brea Hill ( kw, Bre, meaning ''hill''), pronounced "Bray Hill" is a round hill beside the River Camel estuary in north Cornwall, England, United KingdomOrdnance Survey: Landranger map sheet 200 ''Newquay & Bodmin'' The hill is highOrdnance Survey: Explorer map (scale 1:25000); Sheet 106 ''Newquay & Padstow'' and there are Bronze Age tumuli (burial mounds) at the summit. The underlying geology in this area of Cornwall is Devonian slates. Brea Hill is situated at the south end of Daymer Bay between the settlements of Trebetherick and Rock in the civil parish of St Minver Lowlands. Cornwall Council online mapping. Retrieved June 2010 approximately five miles northwest of Wadebridge On the west side, Brea Hill rises straight from the foreshore; on the north and south it rises from low sand dunes. To the east, the dunes give way to a golf course and grassland with St Enodoc's Church (where the poet Sir John Betjeman is buried) just below the hill. The South West Coast Path ...
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Polzeath
Polzeath (; kw, Polsegh, meaning ''dry creek'') is a small seaside resort village in the civil parish of St Minver in Cornwall, England, United Kingdom. It is approximately north west of Wadebridge on the Atlantic coast.Ordnance Survey: Landranger map sheet 200 ''Newquay & Bodmin'' Polzeath has a sandy beach and is popular with holiday-makers and surfers. The beach is wide and extends from the seafront at low water; however, most of the sand is submerged at high water. At exceptionally high spring tides the sea floods the car park at the top of the beach. Polzeath beach is patrolled by lifeguards during the summer and is described on the RNLI website as "a wide, flat beach with some shelter from winds, it sees good quality surf and is quite often extremely crowded". Dolphins may sometimes be spotted in the bay and the coastline north of Polzeath is a good area for seeing many types of birds including corn buntings and puffins. The main street runs along the seafront and ...
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Daymer Bay
Daymer Bay is a bay and a beach on the east side of the River Camel estuary in north Cornwall, England, United Kingdom. It is situated approximately six miles (10 km) north of Wadebridge.Ordnance Survey: Landranger map sheet 200 ''Newquay & Bodmin'' Daymer Bay lies west of Trebetherick village at . The bay is bounded to the north by Trebetherick Point and to the south by Brea Hill. Daymer Bay beach is backed by dunes and behind them is St Enodoc's Church where the poet John Betjeman is buried. The beach is very popular for windsurfing and kitesurfing Kiteboarding or kitesurfing is a sport that involves using wind power with a large power kite to pull a rider across a water, land, or snow surface. It combines aspects of paragliding, surfing, windsurfing, skateboarding, snowboarding, and wak .... References External links Daymer Bay tide times Beaches of Cornwall Bays of Cornwall Populated coastal places in Cornwall {{NorthCornwall-geo-stub ...
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John Betjeman
Sir John Betjeman (; 28 August 190619 May 1984) was an English poet, writer, and broadcaster. He was Poet Laureate from 1972 until his death. He was a founding member of The Victorian Society and a passionate defender of Victorian architecture, helping to save St Pancras railway station from demolition. He began his career as a journalist and ended it as one of the most popular British Poets Laureate and a much-loved figure on British television. Life Early life and education Betjeman was born John Betjemann. He was the son of a prosperous silverware maker of Dutch descent. His parents, Mabel (''née'' Dawson) and Ernest Betjemann, had a family firm at 34–42 Pentonville Road which manufactured the kind of ornamental household furniture and gadgets distinctive to Victorians. During the First World War the family name was changed to the less German-looking Betjeman. His father's forebears had actually come from the present day Netherlands more than a century earlier, setting ...
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St Minver Lowlands
St Minver ( kw, Sen Menvra) is the name of an ecclesiastical parish, a civil parish and a village in north Cornwall, England, United Kingdom. The civil parish of St Minver is in Bodmin Registration District and is nominally divided into St Minver Highlands (to the north and east) and St Minver Lowlands (to the west). The combined parish is bounded on the south and west by the estuary of the River Camel, on the north by the Atlantic coast, and on the east by the parishes of St Endellion and St Kew. The population of the parish in the 2001 census was 2,474 (St Minver Highlands 1025; St Minver Lowlands 1449) decreasing to 2,393 at the 2011 census. Settlements The principal villages in the combined parish are the churchtown of St Minver, Rock, Trebetherick and Polzeath. Other settlements include Tredrizzick, Penmean, Splatt, Porthilly, Pityme and Trevanger. St Minver village is centred on a small square at the crossroads of two unclassified roads. It is situated 3 miles ...
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Rock, Cornwall
Rock ( kw, Pennmeyn) is a coastal fishing village in Cornwall, England, United Kingdom. It is opposite Padstow on the north-east bank of the River Camel estuary. The village is in the civil parish of St Minver Lowlands about north-west of Wadebridge.Ordnance Survey: Landranger map sheet 200 ''Newquay & Bodmin'' Ordnance Survey: Explorer map (scale 1:25000); Sheet 106 ''Newquay & Padstow'' Toponymy The original name recorded in 1303 was , Cornish for 'the end or head of stones'. An alternative, ''Blaketorre'' ('Black Tor'), is found in 1337. This had become ''Black Rock'' by the 18th century and was subsequently shortened to Rock. The name of the ferry that operates between Rock and Padstow recalls the old place name. Geography The main residential area is set back from the coast along the road from Pityme and St Minver. To the northeast, Rock is contiguous with the settlements of Splatt and Pityme. Stoptide is a southern extension of Rock. Rock is best known for its estuar ...
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Cornwall
Cornwall (; kw, Kernow ) is a historic county and ceremonial county in South West England. It is recognised as one of the Celtic nations, and is the homeland of the Cornish people. Cornwall is bordered to the north and west by the Atlantic Ocean, to the south by the English Channel, and to the east by the county of Devon, with the River Tamar forming the border between them. Cornwall forms the westernmost part of the South West Peninsula of the island of Great Britain. The southwesternmost point is Land's End and the southernmost Lizard Point. Cornwall has a population of and an area of . The county has been administered since 2009 by the unitary authority, Cornwall Council. The ceremonial county of Cornwall also includes the Isles of Scilly, which are administered separately. The administrative centre of Cornwall is Truro, its only city. Cornwall was formerly a Brythonic kingdom and subsequently a royal duchy. It is the cultural and ethnic origin of the Cornish dias ...
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List Of Places In Cornwall
This is a list of towns and villages in the ceremonial county of Cornwall, United Kingdom. The ceremonial county includes the unitary authorities of Cornwall and the Isles of Scilly. In accordance with gazetteers, Cornish names are in the standard written form approved by the Maga signage panel. For the civil parishes which often share the name of a village, see Civil parishes in Cornwall. A B C D E F Falmouth, Farms Common, Fenton Pits, Fentonadle, Feock, Fernsplatt, Fistral Beach, Fivelanes, Fletchersbridge, Flexbury, Flushing, Fonston, Forder, Forge, Forrabury, Foundry, Four Lanes, Fowey, Foxhole, Fraddam, Fraddon, Freathy, Frogmore, Frogpool, Frogwell G Gam, Gang, Garker, Garras, Georgia, Germoe, Gerrans, Gilbert's Coombe, Gillan, Gloweth, Gluvian, Godolphin Cross, Godrevy, Golant, Golberdon, Goldsithney, Gollawater, Gonamena, Goon Gumpas, Goon Piper, Goonabarn, Goonbell, Goonhavern, Goonhusband, Goonlaze, Goonown, Goonv ...
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St Petroc
Saint Petroc or Petrock ( lat-med, Petrocus; cy, Pedrog; french: link=no, Perreux; ) was a British prince and Christian saint. Probably born in South Wales, he primarily ministered to the Britons of Devon (Dewnans) and Cornwall (Kernow) then forming the kingdom of Dumnonia where he is associated with a monastery at Padstow, which is named after him (Pedroc-stowe, or 'Petrock's Place'). Padstow appears to have been his earliest major cult centre, but Bodmin became the major centre for his veneration when his relics were moved to the monastery there in the later ninth century. Bodmin monastery became one of the wealthiest Cornish foundations by the eleventh century. There is a second ancient dedication to him nearby at Little Petherick or "Saint Petroc Minor". In Devon ancient dedications total a probable seventeen (plus Timberscombe just over the border in Somerset), mostly coastal and including one within the old Roman walls of Exeter as well as the villages of Petrockstowe a ...
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ...
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