Giant's Causeway and Causeway Coast is a World Heritage Site which lies on the Causeway Coast between Causeway Head and Benbane Head, on the north coast of County Antrim, Northern Ireland.

Date and History of Establishment

* National Trust took over ownership in 1961.

* Inscribed on the World Heritage List in 1986.

Area

70 hectares (ha) (of cliffs and foreshore). This does not include the area of the car park, hotel and visitor facilities which are included in the nominated site.

Land Tenure

Some 13 ha were bequeathed in 1961 by its then owner Sir McNaghten to the National Trust and further purchases of freehold and leasehold land were carried out with finance from the Ulster Land Fund. The National Trust now own 70 ha of the cliffs and foreshore, whilst the area of the car park and visitor center is owned by the Moyle District Council. There is also a privately owned hotel. Small sections of the site (containing parts of the cliff top path) are on the private property of a number of individuals.

Altitude

Sea level to 100 meters (m).

Physical Features

The Causeway Coast has an unparalleled display of geological formations representing volcanic activity during the Early Tertiary Period some 50-60 million years ago. Tertiary lavas of the Antrim Plateau, covering some 3,800 square kilometers (km2), represent the largest remaining lava plateau in Europe. The 6 km stretch of coastline comprises a series of headlands and bays, the former consisting of resistant lavas. The average height of the cliffs is 100 m. They have a stepped appearance due to the succession of five or six lava flows through geological time. These geological succession during the Tertiary period, consists of: the Lower Basalts, where about six of the eleven lava flows are 67 m thick and are exposed between Plaiskin Head and Benbane Head; the Interbasaltic Bed which are exposed along extensive sections of the cliffs east of Giant's Causeway; and the Middle Basalts, which are thick flows ranging from 30 m to over 150 m. Specific sites of interest include the Giant's Causeway itself (a sea level promontory of almost entirely regular polygonal columns averaging 45 centimeters (cm) in diameter and numbering approximately 40,000 columns); the Giant's Organ (about sixty 12 m high regular columns; Chimney Tops (a number of columns separated from the cliffs by erosion); and Hamilton's Seat (a view point). The coastline is also cut through by olivine and tholeiite dykes, a good example of which can be seen at Roveran Valley Head. Exposure of these columns, in perfect horizontal sections at such a scale creating a pavement, is considered a unique combination of features.

Climate

Experiences a temperate Atlantic climate.

Vegetation

Over 200 plant species representing a range of habitats covering seashore, cliff, scree, grassland, scrub, heathland and marsh are present. Localized species of note include red broomrape Orobanche alba, sea spleenwort Asplenium marinum and oyster plant Mertemsia maritima.

Fauna

The site is regarded by the Royal Society for the Protection of Birds as one of regional importance within the United Kingdom based on the number of breeding species. Over 50 resident and 30 migrant species have been recorded and include one pair of breeding chough Pyrrhocorax pyrrhocorax and peregrine falcon Falco peregrinus.

Cultural Heritage

The wreck site of the Armada gallesass "Gerona" in Port-na-Spaniagh, below the isolated columns known as the "Chimneys", is of considerable cultural importance. The sub-littoral area is a protected nautical archaeological site, and the treasures and other Armada artifacts recovered by Robert Stenuit and his team between 1967 and 1969 are conserved in the Ulster Museum, Belfast. This collection is a major part of all known recovered Armada artifacts.

The Giant's Causeway featured in the 18th Century geological controversies on the origins of basalts. There is an interesting cultural heritage associated with place names, and other local history such as the kelp (seaweed) and fisheries exploitation carried out by local communities, documented mainly in the 18th to mid-20th centuries.

Local Human Population

The site is uninhabited now, although several small settlements exist immediately inland of the Causeway cliffs. In the 19th century, and up to the acquisition of the site in 1961 by the National Trust, many temporary commercial stalls and huts were either owned or managed by local people for tourists and visitors. A house occupied by a custodian appointed locally to oversee these activities, was located adjacent to the Giant's Causeway.

Visitors and Visitor Facilities

The Causeway is Northern Ireland's most popular tourist attraction with more than 350,000 visitors annually, over half from overseas. In 1883, the first hydro-electric tramway in the world was opened and by 1887 it was extended to the Causeway Head, where two hotels and numbers of guest houses were built. The site figured frequently in 19th century guidebooks and up and till 1961, the area was heavily commercialized. Visitor facilities include car parks and a visitor center which was opened in 1986 and is located at Causeway Head. Public access to the coast is managed by a system of footpaths. The site is annually visited by geology students on field courses, and over 6,000 schoolchildren.

Scientific Research and Facilities

During the last 300 years, the site has been the object of intense study as is evident by the wealth of scientific literature. It was first reported in 1693 and during the 18th century, was central to the debate concerning the origins of igneous rocks. In 1771, Desmarest concluded the Causeway was a lava flow whilst in 1786, Hamilton produced the first detailed analysis. The work of Tomkeieff and Patterson provided descriptions, interpretations and the correct sequence of the lava flows. The former, most notably, proposed descriptive terms for the Causeway jointing which have been internationally adopted for the description of columnar basalts. Biological surveys have been carried out by the National Trust (1985 and 1992).

Conservation Value

The Causeway itself is a unique feature illustrating the geological activity of successive lava flows and interbasaltic beds. Interpretation of this succession has resulted in a detailed analysis of Tertiary events in the North Atlantic. The scientific research carried out on the site has made an important contribution to petrogenesis over a period of nearly 300 years, marking it as a site of great international significance in the history of earth science.

credited to wikipedia and flickr: anadelmann,sandzapple