St David's Head Penmaen Dewi | |
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Coordinates: 51°54′10″N5°18′45″W / 51.902778°N 5.3125°W | |
Location | Pembrokeshire, Wales |
St David's Head (Welsh : Penmaen Dewi) is a headland in the Pembrokeshire Coast National Park, southwest Wales, which marks the divide between the Irish Sea and the Celtic Sea. It is noted for its wildflowers and wildlife, and for the remains of ancient human settlement. The headland and its immediate hinterland are owned by the National Trust, and are accessible to the public by foot via the Pembrokeshire Coast Path.
The westernmost point of mainland Wales, Pen Dal-aderyn, is located just to the south of St David's Head.
St David's Head is situated about 2.5 miles (4 km) northwest of the cathedral city of St David's in Pembrokeshire. This headland marks the narrowest point of St George's Channel, the southern limit of Cardigan Bay and the Irish Sea in Wales, [1] and the northern boundary of the Celtic Sea. There are views to the south of Whitesands Bay, Ramsey Sound (separating Ramsey Island) and St Brides Bay; to the west, of the Bishops and Clerks rocks; and to the east, of the slopes of the large rocky outcrop known as Carn Llidi. [2]
The headland is abundant in wildflowers and wildlife and the waters around it provide a rich habitat for fish, grey seals and porpoises. A variety of seabirds and peregrine falcons are also to be seen. [3]
There are a number of ancient monuments showing signs of early occupation, including an Iron Age cliff fort, prehistoric settlements, a prehistoric defensive wall, signs of various neolithic field systems and Coetan Arthur (Arthur’s Quoit) burial chamber. [4] [5]
Described in a Roman survey of the known world in 140 AD (Ptolemy's Geography) as the 'Promontory of the Eight Perils' (Οκταπιταρον Ακρον - Oktapitaron Akron - in Ptolemy's original Greek).
Tarleton , a slaver of 400 tons burthen, foundered on 28 November 1788 off St David's Head on her fourth slaving voyage from Liverpool to Africa. Her crew was saved. [6]
In 1793, Sir Richard Colt Hoare said in his "Journal of a Tour of South Wales": [7]
"No place could ever be more suited to retirement, contemplation or Druidical mysteries, surrounded by inaccessible rock and open to a wide expanse of ocean. Nothing seems wanting but the thick impenetrable groves of oaks which have been thought concomitant to places of Druidical worship and which, from the exposed nature of this situation, would never, I think, have existed here even in former days."
The Pembrokeshire Coast Path, often called the Pembrokeshire Coastal Path, is a designated National Trail in Pembrokeshire, southwest Wales. Established in 1970, it is a 186-mile (299 km) long-distance walking route, mostly at cliff-top level, with a total of 35,000 feet (11,000 m) of ascent and descent. At its highest point – Pen yr afr, on Cemaes Head – it reaches a height of 574 feet (175 m), and at its lowest point – Sandy Haven crossing, near Milford Haven – it is just 6 feet (2 m) above low water. Whilst most of the coastline faces west, it offers – at varying points – coastal views in every direction of the compass.
Pembrokeshire is a county in the south-west of Wales. It is bordered by Carmarthenshire to the east, Ceredigion to the northeast, and otherwise by the sea. Haverfordwest is the largest town and administrative headquarters of Pembrokeshire County Council.
St Davids or St David's is a cathedral city in Pembrokeshire, Wales. It lies on the River Alun and is part of the community of St Davids and the Cathedral Close. It is the resting place of Saint David, Wales's patron saint, and named after him.
Pembrokeshire Coast National Park is a national park along the Pembrokeshire coast in west Wales.
Skomer or Skomer Island is an island off the coast of Pembrokeshire, in the community of Marloes and St Brides in west Wales. It is well known for its wildlife: around half the world's population of Manx shearwaters nest on the island, the Atlantic puffin colony is the largest in southern Britain, and the Skomer vole is unique to the island. Skomer is a national nature reserve, a Site of Special Scientific Interest and a Special Protection Area. It is surrounded by a marine nature reserve and is managed by the Wildlife Trust of South and West Wales.
Gateholm or Gateholm Island is a small tidal island off the south west coast of Pembrokeshire, in the community of Marloes and St Brides, in the south west side of Wales, in the west of the UK, and about 8 miles (13 km) west of the port of Milford Haven. It is known for its Romano-British remains. Gateholm is owned by the National Trust as part of their Marloes Sands and Mere estate.
Ramsey Island is an island about 1 kilometre off St David's Head in Pembrokeshire on the northern side of St Brides Bay, in southwest Wales, in the community of St Davids and the Cathedral Close. It is 259 hectares in area. Ramsey means Hrafn's island.
Newport is a town, community, electoral ward and ancient port of Parrog, on the Pembrokeshire coast in West Wales at the mouth of the River Nevern in the Pembrokeshire Coast National Park. The town gives its name to Newport Bay.
The Preseli Mountains, also known as the Preseli Hills, or just the Preselis, is a range of hills in western Wales, mostly within the Pembrokeshire Coast National Park and entirely within the county of Pembrokeshire.
Strumble Head is a rocky headland in the community of Pencaer in Pembrokeshire, Wales, within the Pembrokeshire Coast National Park. It marks the southern limit of Cardigan Bay. Three islands lie off the head: Ynys Meicel – 112 feet (34 m) – Ynys Onnen and Carreg Onnen.
Bedd Arthur is a possibly Neolithic hengiform monument megalithic site in the Preseli Hills in the Welsh county of Pembrokeshire. Thirteen upright stones and at least 2 fallen ones, each around 0.6 metres (2.0 ft) high form an oval horseshoe with similarities to the earliest form of Stonehenge.
Prehistoric Wales in terms of human settlements covers the period from about 230,000 years ago, the date attributed to the earliest human remains found in what is now Wales, to the year AD 48 when the Roman army began a military campaign against one of the Welsh tribes. Traditionally, historians have believed that successive waves of immigrants brought different cultures into the area, largely replacing the previous inhabitants, with the last wave of immigrants being the Celts. However, studies of population genetics now suggest that this may not be true, and that immigration was on a smaller scale.
Whitesands Bay is a Blue Flag beach situated on the St David's peninsula in the Pembrokeshire Coast National Park, Wales. Whitesand Bay, on some maps, located 2 miles (3.2 km) west of St. Davids and 1 mile (1.6 km) south of St Davids Head, has been described as the best surfing beach in Pembrokeshire.
Ceibwr Bay is a bay opening into the Irish Sea in Pembrokeshire, west Wales. It is about 7 km west of Cardigan, and 3 km south of the headland of Cemaes Head. A part of it known as the Moyle is owned by the National Trust, and lies within the Pembrokeshire Coast National Park and on the Pembrokeshire Coast Path.
Fishguard and Goodwick is the name of a community that wraps around Fishguard Bay, on the northern coast of Pembrokeshire, Wales. It comprises the two towns of Fishguard and Goodwick, with their neighbourhoods of Dyffryn, Harbour Village, Penyraber, Lower Town, and Stop-and-Call. Within the community are two railway stations and Goodwick Ferry Terminal, which is the terminus of the A40 London to Fishguard Trunk Road.
Cemaes Head is a headland and nature reserve in north Pembrokeshire. It lies in the community of St Dogmaels, within the Pembrokeshire Coast National Park. To the west and north it overlooks Cardigan Bay, and to the east Cardigan Island and the estuary of the River Teifi.
Carn Llidi is a hill east of St David's Head in Pembrokeshire, Wales. Carn Llidi and its surrounding area is part of the Pembrokeshire Coast National Park.
Carnllundain or Carn Llundain is the highest elevation of Ramsey Island in Pembrokeshire, Wales.
The coastline of Wales extends from the English border at Chepstow westwards to Pembrokeshire then north to Anglesey and back eastwards to the English border once again near Flint. Its character is determined by multiple factors, including the local geology and geological processes active during and subsequent to the last ice age, its relative exposure to or shelter from waves, tidal variation and the history of human settlement and development which varies considerably from one place to another. The majority of the coast east of Cardiff in the south, and of Llandudno in the north, is flat whilst that to the west is more typically backed by cliffs. The cliffs are a mix of sandstones, shales and limestones, the erosion of which provides material for beach deposits. Of the twenty-two principal areas which deliver local government in Wales, sixteen have a coastline, though that of Powys consists only of a short section of tidal river some distance from the open sea. Its length has been estimated at 1,680 miles (2,700 km).
The geology of Pembrokeshire in Wales inevitably includes the geology of the Pembrokeshire Coast National Park which extends around the larger part of the county's coastline and where the majority of rock outcrops are to be seen. Pembrokeshire's bedrock geology is largely formed from a sequence of sedimentary and igneous rocks originating during the late Precambrian and the Palaeozoic era, namely the Ediacaran, Cambrian, Ordovician, Silurian, Devonian and Carboniferous periods, i.e. between 635 and 299 Ma. The older rocks in the north of the county display patterns of faulting and folding associated with the Caledonian Orogeny. On the other hand, the late Palaeozoic rocks to the south owe their fold patterns and deformation to the later Variscan Orogeny.
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