Carlingford Lough
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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 ...
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Greencastle, County Down
Greencastle is a castle in County Down, Northern Ireland. While it dates mainly from the 13th century, it had substantial 15th- and 16th-century alterations. It was originally surrounded by outer rectangular walls with four corner towers (ruins of some remain). It is likely to have been built by Hugh de Lacy, along with Carlingford Castle on the opposite side of Carlingford Lough, to guard the narrow entry channel to the Lough, and the ferry crossing between the two. The motte from the earlier Norman, wooden, Motte and Bailey Castle (possibly built by John de Courcey) is still on the seaward side nearer the point. According to one legend John de Courcy was married at Greencastle Castle, but this may have been at the original motte & bailey castle. According to the information boards at the site it was held for the English Crown by Richard de Burgh, Earl of Ulster, from 1264 to 1333. It was attacked and taken by Edward Bruce, the brother of Robert, in 1316. This was in spite of o ...
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Gaeilge
Irish (Standard Irish: ), also known as Gaelic, is a Goidelic language of the Insular Celtic branch of the Celtic language family, which is a part of the Indo-European language family. Irish is indigenous to the island of Ireland and was the population's first language until the 19th century, when English gradually became dominant, particularly in the last decades of the century. Irish is still spoken as a first language in a small number of areas of certain counties such as Cork, Donegal, Galway, and Kerry, as well as smaller areas of counties Mayo, Meath, and Waterford. It is also spoken by a larger group of habitual but non-traditional speakers, mostly in urban areas where the majority are second-language speakers. Daily users in Ireland outside the education system number around 73,000 (1.5%), and the total number of persons (aged 3 and over) who claimed they could speak Irish in April 2016 was 1,761,420, representing 39.8% of respondents. For most of recorded Irish h ...
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Inlet
An inlet is a (usually long and narrow) indentation of a shoreline, such as a small arm, bay, sound, fjord, lagoon or marsh, that leads to an enclosed larger body of water such as a lake, estuary, gulf or marginal sea. Overview In marine geography, the term "inlet" usually refers to either the actual channel between an enclosed bay and the open ocean and is often called an "entrance", or a significant recession in the shore of a sea, lake or large river. A certain kind of inlet created by past glaciation is a fjord, typically but not always in mountainous coastlines and also in montane lakes. Multi-arm complexes of large inlets or fjords may be called sounds, e.g., Puget Sound, Howe Sound, Karmsund (''sund'' is Scandinavian for "sound"). Some fjord-type inlets are called canals, e.g.,  Portland Canal, Lynn Canal, Hood Canal, and some are channels, e.g., Dean Channel and Douglas Channel Douglas Channel is one of the principal inlets of the British C ...
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Lough Swilly
Lough Swilly () in Ireland is a glacial fjord or sea inlet lying between the western side of the Inishowen Peninsula and the Fanad Peninsula, in County Donegal. Along with Carlingford Lough and Killary Harbour it is one of three glacial fjords in Ireland. Geography and ecology Located on the Fanad Peninsula, in County Donegal, the northern extremities of the lough are marked by Fanad Head with its lighthouse and Dunaff Head. Towns situated on the lough include Buncrana on Inishowen and Rathmullan on the western side. At the southern end of the lough lies Letterkenny. In the south of the lough a number of islands (Burt, Inch, Coney, Big Isle) were poldered and the land reclaimed during the 19th century for agriculture and the Londonderry and Lough Swilly Railway constructed embankments on the line from Derry to Letterkenny. These reclaimed lands are now wetlands associated with wildlife conservation and birdwatching, and support over 4,000 whooper swans and thousands of Gre ...
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River Clanrye
Newry River and River Clanrye ( ga, An Rí; Ulster-Scots: ''Clanrye Wattèr'') are names for one of the rivers of Ireland. The river passes through the city of Newry and empties into Carlingford Lough near Warrenpoint. Course The river, which runs through Newry, forms the historic border between County Armagh and County Down. Some maps call the portion downstream from Newry to the Lough the 'Newry River' and the portion upstream of Newry the 'Clanrye' (as it curls around to its sources in the foothills of the Mourne Mountains in Ulster), but not all sources make this distinction. According to local tradition, however, the entire waterway is known as the Clanrye. While the Newry River flows under the Newry Town Hall, according to the Ordnance Survey of Northern Ireland, the Clanrye breaks away from the Newry River near Drummillar. The Clanrye then progresses under the main Belfast to Dublin A1 road at Sheepbridge and onward toward the Mayobridge Road at the Crown Bridges and ...
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Lough Neagh
Lough Neagh ( ) is a freshwater lake in Northern Ireland and is the largest lake in the island of Ireland, the United Kingdom and the British Isles. It has a surface area of and supplies 40% of Northern Ireland's water. Its main inflows come from the Upper River Bann and River Blackwater, and its main outflow is the Lower River Bann. Its name comes from Irish , meaning " Eachaidh's lake".Deirdre Flanagan and Laurance Flanagan, Irish Placenames, (Gill & Macmillan Ltd, 1994) The lough is owned by the Earl of Shaftesbury and managed by Lough Neagh Partnership Ltd. Geography With an area of , it is the British Isles' largest lake by area and is ranked 33rd in the list of largest lakes of Europe. Located west of Belfast, it is about long and wide. It is very shallow around the margins and the average depth in the main body of the lake is about , although at its deepest the lough is about deep. Geology Geologically the Lough Neagh Basin is a depression, built from many t ...
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River Bann
The River Bann (from ga, An Bhanna, meaning "the goddess"; Ulster-Scots: ''Bann Wattèr'') is one of the longest rivers in Northern Ireland, its length, Upper and Lower Bann combined, being 129 km (80 mi). However, the total length of the River Bann, including its path through the 30 km (19 mi) long Lough Neagh is 159 km (99 mi). Another length of the River Bann given is 90 mi. The river winds its way from the southeast corner of Northern Ireland to the northwest coast, pausing in the middle to widen into Lough Neagh. The River Bann catchment has an area of 5,775 km2. The River Bann has a mean discharge rate of 92 m3/s. According to C. Michael Hogan, the Bann River Valley is a settlement area for some of the first human arrivals in Ireland after the most recent glacial retreat. The river has played an important part in the industrialisation in Northern Ireland, especially in the linen industry. Today salmon and eel fisheries are the mo ...
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Canal
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Can ...
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Lough
''Loch'' () is the Scottish Gaelic, Scots and Irish word for a lake or sea inlet. It is cognate with the Manx lough, Cornish logh, and one of the Welsh words for lake, llwch. In English English and Hiberno-English, the anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuaries, straits or bays. Background This name for a body of water is Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish, Manx, and has been borrowed into Lowland Scots, Scottish English, Irish English and Standard English. in origin and is applied to most lakes in Scotland and to many sea inlets in the west and north of Scotland. The word comes from Proto-In ...
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Newry Canal
The Newry Canal, located in Northern Ireland, was built to link the Tyrone coalfields (via Lough Neagh and the River Bann) to the Irish Sea at Carlingford Lough near Newry. It was the first summit level canal to be built in Ireland or Great Britain, and pre-dated the more famous Bridgewater Canal by nearly thirty years and Sankey Canal by fifteen years. It was authorised by the Commissioners of Inland Navigation for Ireland, and was publicly funded. It was opened in 1742, but there were issues with the lock construction, the width of the summit level and the water supply. Below Newry, the Newry Ship Canal was opened in 1769, and both Newry and the canal flourished. By 1800, the canal was in a poor condition, and another £57,000 of public money was spent refurbishing it over the following ten years. Closures during the refurbishment resulted in a loss of traffic, which did not fully recover. In 1829, both canals were transferred to a private company, who spent £80,000 on im ...
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Narrow Water Castle
Narrow Water Castle ( ga, Caisleán an Chaoil; Ulster-Scots: ''Narra Wattèr Castle'') is a 16th-century tower house and bawn near Warrenpoint in Northern Ireland. It is beside the A2 road and on the County Down bank of the Clanrye (Newry) River, which enters Carlingford Lough a mile to the south. It is a historic monument in state care in the townland of Narrow Water, in Newry and Mourne District Council district, at grid ref: J1256 1939. History Originally the site of a 13th century Norman keep (associated with Hugh de Lacy), a replacement tower house and bawn was built at Narrow Water (by the Magennis family) in the 16th century. The replacement structure, built in the 1560s, was a typical example of the tower houses built throughout Ireland at the time. This kind of building, often rectangular in plan and three or more storeys high, comprised a series of superimposed chambers, with stairs, closets and latrines built within the walls (which are 1.5 metres or five ...
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Old Norse
Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their overseas settlements and chronologically coincides with the Viking Age, the Christianization of Scandinavia and the consolidation of Scandinavian kingdoms from about the 7th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid-to-late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse was divided into three dialects: ''Old West Norse'' or ''Old West Nordic'' (often referred to as ''Old Norse''), ''Old East Norse'' or ''Old East Nordic'', and '' Old Gutnish''. Old West Norse and Old East Norse formed a dialect ...
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