This is a list of the Sites of Special Scientific Interest (SSSIs) in the Pembrokeshire Area of Search (AoS). [1]
This is a list of the Sites of Special Scientific Interest (SSSIs) in the Pembrokeshire Area of Search (AoS). [1]
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.
Pembrokeshire Coast National Park is a national park along the Pembrokeshire coast in west Wales.
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.
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.
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.
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