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Landsker Line
The Landsker Line ( cy, Ffin ieithyddol Sir Benfro) is a term used for the language border in Wales between the largely Welsh-speaking and largely English-speaking areas in Pembrokeshire and Carmarthenshire. The English-speaking areas, south of the Landsker line and known as Little England beyond Wales, are notable for having been English linguistically and culturally for many centuries despite being far from the England–Wales border. History During the 11th and 12th centuries both invaders and defenders built more than fifty castles during a complex period of conflict, effectively to consolidate the line. The southernmost was Laugharne; others included Wiston, Camrose, Narberth, and Roch. These are often referred to as "frontier castles" but they were in fact set back a considerable distance from the frontier itself. In the heart of the Normanised colony, the two great fortresses were at Pembroke and Haverfordwest. There were other fortresses within the colony as well, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haverfordwest Castle
Haverfordwest Castle ( cy, Castell Hwlffordd) is a castle located in the town centre at Haverfordwest, Pembrokeshire, south Wales, located in a naturally defensive position at the end of a strong, isolated ridge. The castle was established during Norman times in 1120 but much of the architecture remaining today is dated to 1290. For centuries the castle was an English stronghold. There are several other notable castles in area; Wiston Castle lies to the northeast and Pembroke Castle lies to the south. History Pembrokeshire Records indicate that there was an Iron Age hill fort on the site of the castle although there is no physical evidence to suggest this on the present location. Haverfordwest was believed to have been a Danish settlement prior to the Norman conquest of West Wales in 1093/94. The Flemish settled in the area in 1108 to protect the main Norman stronghold at Pembroke Castle from Welsh raiders from the north. The vast majority of sources indicate that the structur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Taf
The River Taf ( cy, Afon Taf) is a river in West Wales. It rises in the Preseli Hills, Pembrokeshire, and continues through Carmarthenshire to Laugharne. It is one of the three rivers to enter the sea on the east side of Carmarthen Bay. The other two are the River Gwendraeth and River Tywi. Course The River Taf is about from Crymych to Ginst Point, of which about is tidal.The Journal of Conchology 1979 p 7 "CARMARTHEN BAY. Three large estuaries, the Gwendraeth, Afon Tywi and Afon Taf enter the sea on the east side of Carmarthen Bay and these rivers contribute to deposits of muddy shores. Water drains from high ground above the village of Crymych in Pembrokeshire, and at one time flowed at ground level across the main Cardigan–Tenby road ( A478) before falling to the level of the Whitland and Cardigan Railway station Crymmych Arms ( Great Western Railway) where on the UK Ordnance Survey map of 1866 it is shown as the source of the Taf. The stream fulfills its description " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
St Bride’s Bay
St Brides Bay ( cy, Bae Sain Ffraid) is a bay in western Pembrokeshire, West Wales. Either Skomer Island or the mainland extremity of Wooltack Point at the western end of the Marloes Peninsula marks the southern limit of the bay whilst its northern limit is marked by Ramsey Island off St David's Head. The mouth of the bay is about wide and extends some eastwards from this line. Geology The northern and southern shores of the bay are mainly rocky in nature, backed by cliffs up to high. Its eastern shore comprises a series of large and small sandy beaches between rocky sections. The geological exposures around the bay reveal great complexity with considerable folding and faulting of the strata. The cliffs of its southern shore are formed from sandstones of Ordovician and Devonian age together with a suite of both intrusive and extrusive igneous rocks, some of which are Precambrian in age. Those in the north comprise a series of Precambrian and Cambrian age rocks of both sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurence Dudley Stamp
Sir (Laurence) Dudley Stamp, CBE, DSc, D. Litt, LLD, Ekon D, DSc Nat ( – ), was professor of geography at Rangoon and London, and one of the internationally best known British geographers of the 20th century. Educated at King's College London, he specialised in the study of geology and geography and taught at the universities of Rangoon (1923–26) and London (1926–45). From 1936 to 1944 he directed the compilation and publication of the report of the Land Utilisation Survey of Britain. He worked on many official enquiries into the use of land and planning. Early life and education Stamp was born in Catford, London, in 1898, the seventh child of a shopkeeper; his elder brother Josiah became the banker Lord Stamp of Shortlands. He attended University School, Rochester (1910–13), where he joined the Rochester and District Natural History Society. He then studied for a BSc at King's College London, graduating with first-class honours in 1917. Following military service he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Wales
South Wales ( cy, De Cymru) is a loosely defined region of Wales bordered by England to the east and mid Wales to the north. Generally considered to include the historic counties of Glamorgan and Monmouthshire, south Wales extends westwards to include Carmarthenshire and Pembrokeshire. In the western extent, from Swansea westwards, local people would probably recognise that they lived in both south Wales and west Wales. The Brecon Beacons National Park covers about a third of south Wales, containing Pen y Fan, the highest British mountain south of Cadair Idris in Snowdonia. A point of some discussion is whether the first element of the name should be capitalised: 'south Wales' or 'South Wales'. As the name is a geographical expression rather than a specific area with well-defined borders, style guides such as those of the BBC and ''The Guardian'' use the form 'south Wales'. In a more authoritative style guide, the Welsh Government, in their international gateway website, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carmarthen Bay
Carmarthen Bay ( cy, Bae Caerfyrddin) is an inlet of the South Wales coast, including notable beaches such as Pendine Sands and Cefn Sidan sands. Carmarthen Bay is partially within the Pembrokeshire Coast National Park. The Joint Nature Conservation Committee list Carmarthen Bay and Estuaries as a Special Area of Conservation. Geography The River Loughor flows into the bay at the Burry estuary, and the rivers Tywi, Taf and Gwendraeth flow into the bay at the Three Rivers Estuary. Caldey Island lies in the bay near Tenby. The northwestern corner of the bay is separately named as Saundersfoot Bay. Towns and villages in the bay include, from east to west: Llanelli, Burry Port (''Porth Tywyn''), Pembrey (''Penbre''), Kidwelly (''Cydweli''), Ferryside (''Glanyfferi''), Llansteffan, Laugharne (''Talacharn''), Pendine (''Pentywyn''), Amroth, Wisemans Bridge (''Pont-yr-ŵrddoeth''), Saundersfoot and Tenby (''Dinbych y Pysgod''). There are fine beaches at Pendine Sands, Cefn Sidan, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
St Bride's Bay
St Brides Bay ( cy, Bae Sain Ffraid) is a bay in western Pembrokeshire, West Wales. Either Skomer Island or the mainland extremity of Wooltack Point at the western end of the Marloes Peninsula marks the southern limit of the bay whilst its northern limit is marked by Ramsey Island off St David's Head. The mouth of the bay is about wide and extends some eastwards from this line. Geology The northern and southern shores of the bay are mainly rocky in nature, backed by cliffs up to high. Its eastern shore comprises a series of large and small sandy beaches between rocky sections. The geological exposures around the bay reveal great complexity with considerable folding and faulting of the strata. The cliffs of its southern shore are formed from sandstones of Ordovician and Devonian age together with a suite of both intrusive and extrusive igneous rocks, some of which are Precambrian in age. Those in the north comprise a series of Precambrian and Cambrian age rocks of both sedi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
George Owen Of Henllys
George Owen of Henllys (1552 – 26 August 1613) was a Welsh antiquarian, author, and naturalist. Early life George Owen was the eldest son born to Elizabeth Herbert and William Owen in Henllys of the parish of Nevern, near Newport, Pembrokeshire. William Owen ( 1486–1574) was a successful Welsh lawyer who purchased the Lordship of Kemys. Following his father's death, he inherited the estate. Lordship of Kemys George Owen was educated in law at the Inns of Court in London. He spent considerable time fighting a series of lawsuits against family enemies in the county over ownership of manorial franchises. Wales historian During his life span he collected antiquarian information about Wales, including the heraldry, genealogy and historical buildings and structures. He also studied the topography of the county of Pembrokeshire and other parts of Wales. During his studies he performed observations of the geology of Wales, including the strata of limestone and coal. Although he d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richard Fenton
Richard Fenton (January 1747 – November 1821) was a Welsh lawyer, topographer and poet. Biography Fenton was born in January 1747 in St David's, Pembrokeshire, and was baptised in St David's Cathedral on 20 February 1747, "being then a month old". He was educated at the cathedral school, and at an early age obtained a situation in London in the custom house. Later he entered the Middle Temple, and studied for the legal profession. After being called to the bar he attended the circuits in Wales for several years. Subsequently he devoted his time to literary pursuits; he was a friend of Oliver Goldsmith and Sir Richard Colt Hoare. He travelled throughout Wales, studying local records and publishing several topographical volumes. After a merchant uncle died, he took over his mercantile fleet. Fenton died at his home at Plas Glynamel, Fishguard, in November 1821, and was buried nearby at Manorowen. Works Fenton's works include: * ''Poems'', London 1773; 2 vols. 1790. * ''A Histo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Welsh Speakers In The 2011 Census
Welsh may refer to: Related to Wales * Welsh, referring or related to Wales * Welsh language, a Brittonic Celtic language spoken in Wales * Welsh people People * Welsh (surname) * Sometimes used as a synonym for the ancient Britons (Celtic people) Animals * Welsh (pig) Places * Welsh Basin, a basin during the Cambrian, Ordovician and Silurian geological periods * Welsh, Louisiana, a town in the United States * Welsh, Ohio, an unincorporated community in the United States See also * Welch (other) * * * Cambrian + Cymru Wales ( cy, Cymru ) is a country that is part of the United Kingdom. It is bordered by England to the east, the Irish Sea to the north and west, the Celtic Sea to the south west and the Bristol Channel to the south. It had a population in 202 ... {{Disambiguation Language and nationality disambiguation pages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Preseli Hills
The Preseli Hills or, as they are known locally and historically, Preseli Mountains, (Welsh: ''Mynyddoedd y Preseli / Y Preselau'' , ) is a range of hills in western Wales, mostly within the Pembrokeshire Coast National Park. The range stretches from the proximity of Newport in the west to Crymych in the east, some in extent. The highest point at above sea level is Foel Cwmcerwyn. The ancient of track along the top of the range is known as the Golden Road. The Preselis have a diverse ecosystem, many prehistoric sites, and are a popular tourist destination. There are scattered settlements and small villages; the uplands provide extensive unenclosed grazing, and the lower slopes are mainly enclosed pasture. Slate quarrying was once an important industry. More recently, igneous rock is being extracted. The Preselis have Special Area of Conservation status, and there are three sites of special scientific interest (SSSIs). Name variations A peak is spelt ''Percelye'' on a 15 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
