List of Sites of Special Scientific Interest in Pembrokeshire

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Map of Pembrokeshire within Wales Pembrokeshire UK location map.svg
Map of Pembrokeshire within Wales

This is a list of the Sites of Special Scientific Interest (SSSIs) in the Pembrokeshire Area of Search (AoS). [1]

Sites

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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.

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Pembrokeshire Coast National Park is a national park along the Pembrokeshire coast in west Wales.

<span class="mw-page-title-main">Preseli Mountains</span> Hill range in Wales

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<span class="mw-page-title-main">Diocese of St Davids</span> Anglican diocese of the Church in Wales

The Diocese of St Davids is a diocese of the Church in Wales, a church of the Anglican Communion. The diocese covers the historic extent of Ceredigion, Carmarthenshire and Pembrokeshire, together with a small part of western Glamorgan. The episcopal see is the Cathedral Church of St David in the City of St Davids, Pembrokeshire. The present cathedral, which was begun in 1181, stands on the site of a monastery founded in the 6th century by Saint David.

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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. "Find protected areas of land and sea". Natural Resources Wales . Retrieved 9 January 2022.