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.
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.
Cilgerran is both a village, a parish, and also a community, situated on the south bank of the River Teifi in Pembrokeshire, Wales. It was formerly an incorporated market town.
Neyland is a town and community in Pembrokeshire, Wales, lying on the River Cleddau and the upstream end of the Milford Haven estuary. The Cleddau Bridge carrying the A477 links Pembroke Dock with Neyland.
Bluestone is a cultural or commercial name for a number of natural dimension or building stone varieties, including:
Preseli Pembrokeshire was a seat and constituency of the House of Commons of the Parliament of the United Kingdom.
Abereiddy is a hamlet in the county of Pembrokeshire, in west Wales.
Trefin, formerly anglicised as Trevine, is a village in North Pembrokeshire, south-west Wales. The village lies within the parish and community of Llanrhian, which has a significant Welsh-speaking population.
The existence of a slate industry in Wales is attested since the Roman period, when slate was used to roof the fort at Segontium, now Caernarfon. The slate industry grew slowly until the early 18th century, then rapidly during the Industrial Revolution in Wales until the late 19th century, at which time the most important slate producing areas were in northwest Wales. These sites included the Penrhyn Quarry near Bethesda, the Dinorwic Quarry near Llanberis, the Nantlle Valley quarries, and Blaenau Ffestiniog, where the slate was mined rather than quarried. Penrhyn and Dinorwig were the two largest slate quarries in the world, and the Oakeley mine at Blaenau Ffestiniog was the largest slate mine in the world. Slate is mainly used for roofing, but is also produced as thicker slab for a variety of uses including flooring, worktops and headstones.
The geology of Wales is complex and varied; its study has been of considerable historical significance in the development of geology as a science. All geological periods from the Cryogenian to the Jurassic are represented at outcrop, whilst younger sedimentary rocks occur beneath the seas immediately off the Welsh coast. The effects of two mountain-building episodes have left their mark in the faulting and folding of much of the Palaeozoic rock sequence. Superficial deposits and landforms created during the present Quaternary period by water and ice are also plentiful and contribute to a remarkably diverse landscape of mountains, hills and coastal plains.
Solva is a village, community and electoral ward in Pembrokeshire, Wales. The village comprises principally Lower Solva and Upper Solva. The community also includes Middle Mill and Whitchurch.
Narrow-gauge railways were used extensively in the slate industry of Great Britain, especially in Wales. Many quarries had internal tramways, some using many dozens of miles of track. Others had private lines that stretched from the quarry to transhipment points on local railways, rivers, roads or coastal ports.
Croes-goch is a village in North Pembrokeshire, West Wales. It is situated on the A487 between Fishguard and St David's. It lies some five miles northeast of St Davids on the junction of the A487 St Davids to Fishguard road with the B4330 Llanrhian to Haverfordwest. The village, which has a population of about 400, lies within Llanrhian Community Council and lies two miles south of the Pembrokeshire Coast National Park.
Llanrhian is a small village, community and parish in Pembrokeshire in west Wales, near the coast, south of Porthgain village. The community of Llanrhian includes the settlements of Llanhowell, Croesgoch, Portheiddy, Porthgain and Trefin. The village church is St Rhian’s and is of medieval origin. The village is in the Pembrokeshire Coast National Park.
Abermawr is a stretch of coastline and is regarded as a Site of Special Scientific Interest in Pembrokeshire, Wales. Abermawr is a mostly shingle beach with marsh and woodland behind it. It is popular with many walkers who are walking along the coast past Porthgain, Abereiddi and Abercastle. The large pebble bank of the bay was created by a storm on 25 October 1859. The currents at Abermawr can be hazardous but the headlands are low so are less gusty.
The natural resources of Wales have contributed substantially to the economic wealth of the United Kingdom from pre-Roman times to the present. Wales has a complex and varied geology with a wealth of natural minerals. Although Wales has been strongly associated with the coal industry, it has also been the world's leading supplier of slate and of copper at different times. The country lies along the western side of Great Britain and is buffeted by the prevailing South-Westerly trade winds which bring year round rain and wind but also maintain an equable temperate climate. The combination of climate and physical geography and geology have given rise to many different types of landscape and biomes rich in species variety.
The Cwm Ebol quarry was a slate quarry about 1 mile (1.6 km) north west of the village of Pennal in Mid Wales. It operated from about 1860 to about 1906. It was the last Welsh slate quarry connected only to a trans-shipment point instead of directly to a railway.
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.
