List of schools in Pembrokeshire

Last updated

This is a list of schools in Pembrokeshire in Wales.

Contents

English-medium primary schools

Welsh medium primary schools

Secondary schools

Welsh medium secondary schools

Special schools

Independent schools

Further education colleges

Related Research Articles

<span class="mw-page-title-main">Pembrokeshire Coast Path</span> Hiking trail in Wales

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.

<span class="mw-page-title-main">Pembrokeshire</span> County and historic county in Wales

Pembrokeshire is a county in the south-west of Wales. It is bordered by Carmarthenshire to the east, Ceredigion to the northeast, and the rest by sea. The county is home to Pembrokeshire Coast National Park. The Park occupies more than a third of the area of the county and includes the Preseli Hills in the north as well as the 190-mile (310 km) Pembrokeshire Coast Path.

<span class="mw-page-title-main">Haverfordwest</span> Human settlement in Wales

Haverfordwest is the county town of Pembrokeshire, Wales, and the most populous urban area in Pembrokeshire with a population of 14,596 in 2011. It is also a community, being the second most populous community in the county, with 12,042 people, after Milford Haven. The suburbs include the former parish of Prendergast, Albert Town and the residential and industrial areas of Withybush.

<span class="mw-page-title-main">Neyland</span> Human settlement in Wales

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.

<span class="mw-page-title-main">River Cleddau</span> River in Wales

The River Cleddau consists of the Eastern and Western Cleddau rivers in Pembrokeshire, west Wales. They unite to form the Daugleddau estuary and the important harbour of Milford Haven.

Maenclochog is a village, parish and community in Pembrokeshire, south-west Wales. It is also the name of an electoral ward comprising a wider area of four surrounding communities. Maenclochog Community includes the small settlement of Llanycefn and the village of Rosebush.

<span class="mw-page-title-main">Ysgol Bro Gwaun</span> Comprehensive school in Fishguard, Pembrokeshire, Wales

Ysgol Bro Gwaun is a secondary comprehensive school in the town of Fishguard in north Pembrokeshire. It is a predominantly English-medium school with significant use of Welsh, and has a catchment area covering the towns of Fishguard and Goodwick, the villages of Scleddau, Letterston and Newport and the surrounding areas including the Gwaun valley.

<span class="mw-page-title-main">Cwm Gwaun</span> Human settlement in Wales

Cwm Gwaun is a community and valley in north Pembrokeshire, Wales. The community is centred around Pontfaen, a parish and hamlet 4 miles (6.4 km) southeast of Fishguard, and includes the ancient parish of Llanychaer. In 2011, the population was 313. The valley is known for its unspoilt nature and old-world pub, and there are numerous other listed buildings.

<span class="mw-page-title-main">Prendergast, Pembrokeshire</span> Human settlement in Wales

Prendergast is a former village and parish in Pembrokeshire, Wales, now a suburb of Haverfordwest, Pembrokeshire's county town. The name survives as an electoral ward of Haverfordwest. The Western Cleddau forms the parish's western boundary, and the Hiog, a tributary of the Cleddau, the eastern boundary.

<span class="mw-page-title-main">Cuisine of Pembrokeshire</span>

Pembrokeshire has been called "the cottage garden of Wales", due to its good soil and the beneficial effects of the Gulf Stream, which provide a mild climate and a longer growing season than other parts of the country. The good climate and soil meant that the south of the peninsula was coveted by the Norsemen and Normans because it had "great plentie" of corn and cattle The county has prime agricultural land, much of which is located at about 70m above sea level, while to the north, the Preseli Hills rise to 500m above sea level and form uplands that are made up of heather and bracken, which are used for grazing sheep. Consequently, Pembrokeshire is classed as one of the most fertile counties in Wales, with its 392,300 agricultural acres having 14% of its land classed as of good quality, 67% being classed as medium quality and 19% being classed as poor quality. However, agricultural production is subject to market forces and in the 1890s, as a result of the Panic of 1893, a deep agricultural depression led to the area under cultivation falling by a third. Many labourers and farmers had no option but to emigrate to the New World and many of the large farming estates were sold. World War I brought prosperity again, but by the 1930s, as a result of the Great Depression, there was another agricultural depression which lasted until World War II. During the Post-war period agriculture has benefited from marketing schemes and marketing boards, which have helped in the regulation, marketing and distribution of the county's agricultural production.

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.

References

  1. "Home". Nant-y-Cwm School. 14 March 2017.
  2. "Redhill High School – Clynderwen".