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St Enodoc's Church, Trebetherick

All accuracy disputesChurch of England church buildings in CornwallEnglish Gothic architecture in CornwallGrade I listed churches in Cornwall
St Enodoc's Church, Trebetheric, Cornwall 01
St Enodoc's Church, Trebetheric, Cornwall 01

St. Enodoc Church, Trebetherick (Old Cornish: 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 (grid reference SW931772). It is a Grade I listed building.

Excerpt from the Wikipedia article St Enodoc's Church, Trebetherick (License: CC BY-SA 3.0, Authors, Images).

St Enodoc's Church, Trebetherick
Daymer Lane,

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N 50.5581 ° E -4.9215 °
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St Enodoc

Daymer Lane
PL27 6SA , St. Minver Lowlands
England, United Kingdom
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St Enodoc's Church, Trebetheric, Cornwall 01
St Enodoc's Church, Trebetheric, Cornwall 01
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Brea Hill
Brea Hill

Brea Hill (Cornish: Bre, meaning hill), pronounced "Bray Hill" is a round hill beside the River Camel estuary in north Cornwall, England, United Kingdom The hill is 62 metres (203 ft) high 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. approximately five miles northwest of WadebridgeOn 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. Brea Hill is within the Rock Dunes SSSI (Site of Special Scientific Interest). The reason that Brea Hill is such a positive feature in the landscape is that the centre of the hill, west to east, is a dolerite dyke, well-seen from the beach on the west and in the quarry on the east slope and in both exposures soft-sediment deformation is seen implying the intrusion followed shortly after deposition of the material which later became slate during the Variscan Orogeny. The dyke is shown on the British Geological Survey map Sheets 335 and 336, and memoir, for the Geology around Trevose Head and Camelford. The South West Coast Path follows the west flank of the hill with an alternative route passing to the east. Brea Hill is grassed and treeless (except for a small wooded area low on the south flank) with rough footpaths leading to the summit and burial mounds.

Polzeath
Polzeath

Polzeath (;Standard Written Form: 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 6 miles (9.7 km) north west of Wadebridge on the Atlantic coast.Polzeath has a sandy beach and is popular with holiday-makers and surfers. The beach is 1,500 feet (460 m) wide and extends 1,200 feet (370 m) 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, particularly on migration but also including occasional puffins nesting on the offshore islands.The main street runs along the seafront and has a parade of shops catering for holidaymakers and residents. There are pubs, cafés, restaurants, a caravan site and several camping sites in the immediate area. The road rises up steep hills at both ends of the seafront, towards the village of Trebetherick to the southwest and New Polzeath to the northeast. The South West Coast Path runs from Daymer Bay in the South through Polzeath and up to Pentire Head in the North.

Doom Bar
Doom Bar

The Doom Bar (previously known as Dunbar sands, Dune-bar, and similar names) is a sandbar at the mouth of the estuary of the River Camel, where it meets the Celtic Sea on the north coast of Cornwall, England. Like two other permanent sandbanks further up the estuary, the Doom Bar is composed mainly of marine sand that is continually being carried up from the seabed. More than 60 percent of the sand is derived from marine shells, making it an important source of agricultural lime, which has been collected for hundreds of years; an estimated 10 million tons of sand or more has been removed from the estuary since the early nineteenth century, mainly by dredging. The estuary mouth, exposed to the Atlantic Ocean, is a highly dynamic environment, and the sands have been prone to dramatic shifts during storms. According to tradition, the Doom Bar formed in the reign of Henry VIII, damaging the prosperity of the port of Padstow a mile up the estuary. Until the twentieth century, access to Padstow's harbour was via a narrow channel between the Doom Bar and the cliffs at Stepper Point, a difficult passage for sailing ships to navigate, especially in north-westerly gales when the cliffs would cut off the wind. Many ships were wrecked on the Doom Bar, despite the installation of mooring rings and capstans on the cliffs and quarrying away part of Stepper Point to improve the wind. In the early twentieth century the main channel moved away from the cliffs, and continued dredging has made it much safer for boats, but deaths have occurred on the bar as recently as May 2020.A Cornish folklore legend relates that a mermaid created the bar as a dying curse on the harbour after she was shot by a local man. The Doom Bar has been used in poetry to symbolise feelings of melancholy, and has given its name to the flagship ale from the local Sharp's Brewery.