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Ogmore-by-Sea
Ogmore-by-Sea ( Welsh: ''Aberogwr'', meaning "Mouth of the River Ogmore") is a seaside village in St Brides Major community in the Vale of Glamorgan, Wales. It lies on the western limit of the Glamorgan Heritage Coast of south Wales. The population in 2011 was 878. History A polished flint axe-head of Seamer type was found at Ogmore Mill in 1976. Just like its counterparts in Cornwall, Ireland and Brittany, the west-facing beach and coast was notorious as a graveyard for ships during strong on-shore winds (south-westerly winds from the Atlantic). Many ships, in particular, were destroyed on Tusker Rock, a brutal reef slightly out to sea that is totally covered at high tide. There are urban legends of organised shipwrecking at Ogmore (and all across the Vale of Glamorgan coastline) like tales from Cornwall of the use of false lights so that passing ships would mistake a flickering light as a lighthouse or ship at anchor and be lured to destruction, but there is no historic ...
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Ogmore-by-Sea - Geograph
Ogmore-by-Sea ( Welsh: ''Aberogwr'', meaning "Mouth of the River Ogmore") is a seaside village in St Brides Major community in the Vale of Glamorgan, Wales. It lies on the western limit of the Glamorgan Heritage Coast of south Wales. The population in 2011 was 878. History A polished flint axe-head of Seamer type was found at Ogmore Mill in 1976. Just like its counterparts in Cornwall, Ireland and Brittany, the west-facing beach and coast was notorious as a graveyard for ships during strong on-shore winds (south-westerly winds from the Atlantic). Many ships, in particular, were destroyed on Tusker Rock, a brutal reef slightly out to sea that is totally covered at high tide. There are urban legends of organised shipwrecking at Ogmore (and all across the Vale of Glamorgan coastline) like tales from Cornwall of the use of false lights so that passing ships would mistake a flickering light as a lighthouse or ship at anchor and be lured to destruction, but there is no historic ...
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St Brides Major (community)
St Brides Major ( cy, Sant-y-Brid) is a community on the western edge of the Vale of Glamorgan, South Wales. Its largest settlement is the village of St Brides Major, and also includes the villages of Ogmore-by-Sea and Southerndown, and the hamlets of Ogmore Village, Castle-upon-Alun, Heol-y-Mynydd, Norton and Pont-yr-Brown It is notable for coastal geology and scenery, limestone downlands and fossilised primitive mammals, sea cliffs and beaches, two Iron Age hillforts, three medieval castle sites, (one, Ogmore Castle, still extant), two stepping stone river crossings and a clapper bridge. Three long distance paths cross the community. It is the western limit of the Vale of Glamorgan Heritage Coast, and has a visitor centre and tourist facilities. Geology and Landscape of south-west facing coastline forms one side of the community. This is an SSSI and part of the Vale of Glamorgan Heritage Coast, with rocky limestone cliffs, broad sandy beaches and deeply fissured wave-cut pl ...
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River Ogmore
The River Ogmore ( cy, Afon Ogwr) is a river in South Wales that is popular with anglers. It runs generally from north to south from the Ogmore Vale and Gilfach Goch, past Bridgend and Ogmore. The River Ogmore rises at Craig Ogwr (527 m) in the Ogmore Valley as the Ogwr Fawr before it links with the Ogwr Fach at Blackmill. The River Llynfi, the River Garw and finally the River Ewenny in its estuary are all tributaries of the Ogmore which flows into the sea between Ogmore-by-Sea and the Merthyr Mawr sand-dunes. Geology and geography The Ogmore has two major branches in its headwaters: the which flows south through Nantymoel, Ogmore Vale and Lewistown; and joining it from the east the which flows through . After the confluence with the , they join to form the at Blackmill. Most of the headwaters flow over Carboniferous coal measures overlain by glacial drift and fluvial gravels. The valleys are reasonably broad for a small river, and many of the tributaries meand ...
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Vale Of Glamorgan
The Vale of Glamorgan ( cy, Bro Morgannwg ), often referred to as The Vale, is a county borough in the south-east of Wales. It borders Bridgend County Borough to the west, Cardiff to the east, Rhondda Cynon Taf to the north, and the Bristol Channel to the south. With an economy based largely on agriculture and chemicals, it is the southernmost unitary authority in Wales. Attractions include Barry Island Pleasure Park, the Barry Tourist Railway, Medieval wall paintings in St Cadoc's Church, Llancarfan, Porthkerry Park, St Donat's Castle, Cosmeston Lakes Country Park and Cosmeston Medieval Village. The largest town is Barry. Other towns include Penarth, Llantwit Major, and Cowbridge. There are many villages in the county borough. History The area is the southernmost part of the county of Glamorgan. Between the 11th century and 1536 the area was part of the Lordship of Glamorgan. In medieval times, the village of Cosmeston, near what is today Penarth in the south eas ...
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Southerndown
Southerndown is a village in southern Wales to the southwest of Bridgend, in St Brides Major community, close to Llantwit Major and Ogmore-by-Sea. It is mostly known for its beach which backs Dunraven Bay (Welsh: ''Bae Dwnrhefn''), which is a popular tourist destination during the summer months and since 1972 has been part of a Heritage Coast and is part of the Southerndown Coast SSSI. When the tide is out there is an expanse of sand and pools. The cliffs are an obvious example of sedimentary rock. Beach As Southerndown, along with nearby Ogmore-by-Sea, is a west-facing beach (and hence on the Atlantic coast), off-shore winds usually generate much good-quality surf, helped by the warming effects of the Gulf Stream. A larger rocky shore platform and beach to the southeast is separated by a headland on which are the remains of Dunraven Castle (Welsh: Castell Dwnrhefn). This beach is lesser used for inconvenience and severing of its land link — it has access by steep s ...
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Glamorgan Heritage Coast
The Glamorgan Heritage Coast is a stretch of coastline in the Vale of Glamorgan, South Wales, UK. The Glamorgan Heritage Coast lies between Ogmore-by-Sea and St Athan (with Nash Point at its midpoint) on the South Wales coast. There is a Heritage Coast Centre located at Dunraven Park, Southerndown, at the western end of the coast, providing an information point and education centre. The coast includes the Southerndown Coast Site of Special Scientific Interest at its heart, a section from Ogmore-by-Sea, particularly interesting for its exposed Triassic alluvial fan deposits of carboniferous limestone. There is an Iron Age promontory fort (as well as a 19th-century lighthouse) at Nash Point and an ancient cairn or cromlech at Cwm Marcross. The stretch of coast made the news in 2014 when coastal erosion Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, ...
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Tusker Rock
Tusker Rock ( cy, Ynys Twsgr), is a rock in the Bristol Channel, about west of Ogmore-by-Sea, Vale of Glamorgan, Wales. It is suggested that it takes its name from Tuska the Viking, a Dane whose fellow Vikings semi-colonised the Vale of Glamorgan. Alternatively, the name might derive (as with the similarly named Tuskar Rock, IrelandBilly Colfer ( 2004) ''The Hook Peninsula: County Wexford 'p30Cork University Press and various other Tusker Rocks in the Bristol Channel and Milford Haven/Skomer area) simply from the Old Norse Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their overseas settlemen ... ''tu'' (large) ''skar'' (rock). It is fully visible only at low tide, and was formerly a notorious hazard for ships. Today, the waters around Tusker Rock are a popular diving location. References Extern ...
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Carboniferous Limestone
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian epoch (geology), Epoch of the Carboniferous period (geology), Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup. Depositional basins Within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east–west aligned belt of land stretching through central Wales and the English Midlands to East Anglia and on into Belgium. The limestones deposited to its south form a distinct South Wales-Mendip province which extends from P ...
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Merthyr Mawr
Merthyr Mawr is a village and community in Bridgend, Wales. The village is about 2½ miles from the centre of Bridgend town. The population of the community at the 2011 census was 267. The community occupies the area west of the Ewenny River, between Bridgend and Porthcawl. It takes in the settlement of Tythegston and a stretch of coastal sand dunes known as Merthyr Mawr Warren. It is in the historic county of Glamorgan. Buildings and landmarks of note Merthyr Mawr House is an early 19th-century mansion built by Sir John Nicholl and set in an extensive park. Within the park is the Iron Age hillfort known as Chapel Hill Camp, and within the embankments is the now roofless 15th century chapel of St Roque (or Roch), which houses two early medieval inscribed stones.
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Bridgend
Bridgend (; cy, Pen-y-bont ar Ogwr or just , meaning "the end of the bridge on the Ogmore") is a town in Bridgend County Borough in Wales, west of Cardiff and east of Swansea. The town is named after the medieval bridge over the River Ogmore. The River Ewenny also flows through the town. The population was 49,597 in 2021. Historically a part of Glamorgan, Bridgend has greatly expanded in size since the early 1980s – the 2001 census recorded a population of 39,429 for the town and the 2011 census reported that the Bridgend Local Authority had a population of 139,200 – up from 128,700 in 2001. This 8.2% increase was the largest increase in Wales except for Cardiff. The town is undergoing a redevelopment project, with the town centre mainly pedestrianised and ongoing works including Brackla Street Centre redevelopment to Bridgend Shopping Centre, Rhiw Car Park redevelopment, ongoing public realm improvements and the upgrade of the Bridgend Life Centre and demolition ...
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Ireland
Ireland ( ; ga, Éire ; Ulster Scots dialect, Ulster-Scots: ) is an island in the Atlantic Ocean, North Atlantic Ocean, in Northwestern Europe, north-western Europe. It is separated from Great Britain to its east by the North Channel (Great Britain and Ireland), North Channel, the Irish Sea, and St George's Channel. Ireland is the List of islands of the British Isles, second-largest island of the British Isles, the List of European islands by area, third-largest in Europe, and the List of islands by area, twentieth-largest on Earth. Geopolitically, Ireland is divided between the Republic of Ireland (officially Names of the Irish state, named Ireland), which covers five-sixths of the island, and Northern Ireland, which is part of the United Kingdom. As of 2022, the Irish population analysis, population of the entire island is just over 7 million, with 5.1 million living in the Republic of Ireland and 1.9 million in Northern Ireland, ranking it the List of European islan ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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