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Old Bridge, Bridgend
The Old Bridge ( cy, Yr Hen Bont) is a medieval two arched stone footbridge that spans the River Ogmore at Bridgend in Wales. It is not known who designed or built the bridge, however it was built in approximately 1425. The bridge was repaired in 1775 and restored both in 2005 and 2011. The bridge is a scheduled ancient monument and a grade II* listed bridge. History and construction The Old Bridge replaced an earlier medieval structure spanning the River Ogmore. The name of Bridgend in Welsh is ''Pen-y-bont ar Ogwr'', which means "the head of the bridge on the Ogmore". Pilgrims would have used the bridge to cross the River Ogmore on their way to St David's Cathedral. The stone bridge is believed to have been built around 1425 with five-spans. It is not known who designed and built the bridge. The five-span structure had three river arches and smaller flood arches on each bank. On 21 August 1775, the western pier had been demolished due to a flood, which partially destroyed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 meander ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridgend The Old Bridge Stone Plaque 2275113 7f690eb4
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 of S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scheduled Monuments In Wales
Scheduled monuments (also known as scheduled ancient monuments, or SAMs) are sites of archaeological importance with specific legal protection against damage or development. The list of such monuments in Wales is maintained by Cadw: Welsh Historic Monuments, an executive agency within the Welsh National Assembly. there were 4,186 scheduled monuments in Wales, distributed among all 22 principal areas of Wales. 39 sites cross a border between two authorities, (ridge-top cairns, bridges and aqueducts, cross dykes, tramroads) so are included in both lists. The lists below show these sites, arranged by principal areas (counties and county boroughs), and in the case of the larger counties, sub-divided to maintain a manageable number of sites per page. Lists of scheduled monuments * List of scheduled monuments in Blaenau Gwent (13 sites) * List of scheduled monuments in Bridgend (59 sites) * List of scheduled monuments in Caerphilly (46 sites) * List of scheduled monuments in Cardiff ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pedestrian Bridges In Wales
A pedestrian is a person traveling on foot, whether walking or running. In modern times, the term usually refers to someone walking on a road or pavement, but this was not the case historically. The meaning of pedestrian is displayed with the morphemes ''ped-'' ('foot') and ''-ian'' ('characteristic of'). This word is derived from the Latin term ''pedester'' ('going on foot') and was first used (in English language) during the 18th century. It was originally used, and can still be used today, as an adjective meaning plain or dull. However, in this article it takes on its noun form and refers to someone who walks. The word pedestrian may have been used in middle French in the Recueil des Croniques et Anchiennes Istories de la Grant Bretaigne, à présent nommé Engleterre. In California the definition of a pedestrian has been broadened to include anyone on any human powered vehicle that is not a bicycle, as well as people operating self-propelled wheelchairs by reason of ph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Bridges In The United Kingdom In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] |
