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Cranfield Point
Cranfield Point ( ga, Pointe Chreamhchoille) is the southernmost point of Northern Ireland. It is located at the mouth of Carlingford Lough in the townland of Cranfield, County Down. It was once the site of the Cranfield Point lighthouse, marking the entrance to the lough. Its poor position led to the construction of the Haulbowline Lighthouse situated in the middle of the entrance to Carlingford Lough. Cranfield Point Lighthouse subsequently fell victim to coastal erosion Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward ... and collapsed into the sea during the 1860s. The lighthouse keeper's cottage remained and was later converted into a private residence that can still be seen as of 2007, identified by its characteristic tall black chimneys. References Headlands of County ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cranfield Point Lighthouse - Geograph
Cranfield is a village and civil parish in the west of Bedfordshire, England, situated between Bedford and Milton Keynes. It had a population of 4,909 in 2001. increasing to 5,369 at the 2011 Census. The parish is in Central Bedfordshire unitary authority. It is best known for being the home of Cranfield University and Cranfield Airport (an airfield). The hamlet of Bourne End is located just north of Cranfield, and is part of the civil parish. Wharley End was a separate settlement, but now forms the northern part of Cranfield village, by the university. Amenities Cranfield has two public houses, a football club, coffee shop, dog grooming salon, hairdressers, barbers, several take-away restaurants, one small supermarket and two car dealerships. There is also a surgery and dentist's practice along with a pharmacy. Cranfield has a university, three schools, three parks and a multi-use games area. The village Post Office is now contained within The Co-operative Group store; pre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Extreme Points Of The United Kingdom
This is a list of the extreme points of the United Kingdom: the points that are farther north, south, east or west than any other location. Traditionally the extent of the island of Great Britain has stretched "from Land's End to John o' Groats" (that is, from the extreme southwest of mainland England to the far northeast of mainland Scotland). This article does not include references to the Channel Islands because they are Crown dependencies, not constituent parts of the United Kingdom. Extreme points of the United Kingdom * Northernmost point – Out Stack, Shetland at * Northernmost settlement – Skaw, Unst, Shetland Islands at * Southernmost point – Pednathise Head, Western Rocks, Isles of Scilly at * Southernmost settlement – St Agnes, Isles of Scilly at * Westernmost point – Rockall at , which was only incorporated into Scotland in the 20th century. If Rockall is ignored, Soay, St Kilda, at is the westernmost point. * Westernmost settlement – Belleek ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Ireland
Northern Ireland ( ga, Tuaisceart Éireann ; sco, label= Ulster-Scots, Norlin Airlann) is a part of the United Kingdom, situated in the north-east of the island of Ireland, that is variously described as a country, province or region. Northern Ireland shares an open border to the south and west with the Republic of Ireland. In 2021, its population was 1,903,100, making up about 27% of Ireland's population and about 3% of the UK's population. The Northern Ireland Assembly (colloquially referred to as Stormont after its location), established by the Northern Ireland Act 1998, holds responsibility for a range of devolved policy matters, while other areas are reserved for the UK Government. Northern Ireland cooperates with the Republic of Ireland in several areas. Northern Ireland was created in May 1921, when Ireland was partitioned by the Government of Ireland Act 1920, creating a devolved government for the six northeastern counties. As was intended, Northern Ireland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carlingford Lough
Carlingford Lough (, Ulster Scots: ''Carlinford Loch'') is a glacial fjord or sea inlet in northeastern Ireland, forming part of the border between Northern Ireland to the north and the Republic of Ireland to the south. On its northern shore is County Down, the Mourne Mountains, and the town of Warrenpoint; on its southern shore is County Louth, the Cooley Mountains and the village of Carlingford. The Newry River flows into the loch from the northwest. Name The English name Carlingford and the Irish name ''Loch Cairlinn'' come from the Old Norse ''Kerlingfjǫrðr'', meaning "narrow sea-inlet of the hag" or old woman. This may have referred to the three mountain tops, locally called The Three Nuns, frequently used as pilot points on entering the lough. Its earlier Irish name was ''Snámh Aighneach'', meaning "swift sea-channel". It could also mean "swift swimming-place", referring to a crossing point which could be swum by horses, probably Narrow Water. An older English nam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Townland
A townland ( ga, baile fearainn; Ulster-Scots: ''toonlann'') is a small geographical division of land, historically and currently used in Ireland and in the Western Isles in Scotland, typically covering . The townland system is of Gaelic origin, pre-dating the Norman invasion, and most have names of Irish origin. However, some townland names and boundaries come from Norman manors, plantation divisions, or later creations of the Ordnance Survey.Connolly, S. J., ''The Oxford Companion to Irish History, page 577. Oxford University Press, 2002. ''Maxwell, Ian, ''How to Trace Your Irish Ancestors'', page 16. howtobooks, 2009. The total number of inhabited townlands in Ireland was 60,679 in 1911. The total number recognised by the Irish Place Names database as of 2014 was 61,098, including uninhabited townlands, mainly small islands. Background In Ireland a townland is generally the smallest administrative division of land, though a few large townlands are further divided into h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Down
County Down () is one of the six counties of Northern Ireland, one of the nine counties of Ulster and one of the traditional thirty-two counties of Ireland. It covers an area of and has a population of 531,665. It borders County Antrim to the north, the Irish Sea to the east, County Armagh to the west, and County Louth across Carlingford Lough to the southwest. In the east of the county is Strangford Lough and the Ards Peninsula. The largest town is Bangor, on the northeast coast. Three other large towns and cities are on its border: Newry lies on the western border with County Armagh, while Lisburn and Belfast lie on the northern border with County Antrim. Down contains both the southernmost point of Northern Ireland (Cranfield Point) and the easternmost point of Ireland (Burr Point). It was one of two counties of Northern Ireland to have a Protestant majority at the 2001 census. The other Protestant majority County is County Antrim to the north. In March 2018, ''The Sunda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lighthouse
A lighthouse is a tower, building, or other type of physical structure designed to emit light from a system of lamps and lenses and to serve as a beacon for navigational aid, for maritime pilots at sea or on inland waterways. Lighthouses mark dangerous coastlines, hazardous shoals, reefs, rocks, and safe entries to harbors; they also assist in aerial navigation. Once widely used, the number of operational lighthouses has declined due to the expense of maintenance and has become uneconomical since the advent of much cheaper, more sophisticated and effective electronic navigational systems. History Ancient lighthouses Before the development of clearly defined ports, mariners were guided by fires built on hilltops. Since elevating the fire would improve the visibility, placing the fire on a platform became a practice that led to the development of the lighthouse. In antiquity, the lighthouse functioned more as an entrance marker to ports than as a warning signal for reefs a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haulbowline Lighthouse
The Haulbowline Lighthouse is an active 19th century lighthouse. Described as an "elegant, tapering stone tower" it is located at the entrance to Carlingford Lough, near Cranfield Point in County Down, Northern Ireland. The lighthouse was built on the eastern part of the Haulbowline rocks, one of a number of navigation hazards at the seaward end of Carlingford Lough, which include a notable rocky shoal or bar across the mouth of the lough. The multi-purpose light was designed to help mark the rocks and, when first built, the depth of water over the bar, as well as acting as a landfall light for ships entering from the Irish Sea. Associated with the lighthouse are the leading lights at Green Island and Vidal Bank which mark the safe channel along Carlingford Lough, with Haulbowline displaying a reserve light in case of problems with these leading lights. History Completed in 1824, the lighthouse was designed by George Halpin following complaints made to the Ballast Board, the pre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Erosion
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion commonly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
