Slate River (Ireland)
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Slate River (Ireland)
The Slate River ( ga, An Tarae) or River Slate is a river in County Kildare and County Offaly, Ireland, a tributary of the Figile River. Name Its name derives from the slate quarries in the region. The Irish language name derives from Wiktionary:tarae, ''tarae'', meaning mill race, referring to Sally Corn Mill, Rathangan, County Kildare, Rathangan. The river was historically known as the Clashaghbane River. Course Slate River rises near Ballynafagh Lake in Prosperous, County Kildare, Prosperous and flows southwest, passing under the R403 road (Ireland), R403 road at Graigues. It continues westward parallel to, and north of, the Grand Canal (Ireland), Grand Canal. The Slate passes under the Grand Canal via the Derrymullen aqueduct and is bridged by the R415 road (Ireland), R415 at Littletown. The Slate River continues through Ballyteague Forest and passes by the Lullymore Heritage and Discovery Park on the Bog of Allen. It passes through Rathangan, County Kildare where it passe ...
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County Kildare
County Kildare ( ga, Contae Chill Dara) is a county in Ireland. It is in the province of Leinster and is part of the Eastern and Midland Region. It is named after the town of Kildare. Kildare County Council is the local authority for the county, which has a population of 246,977. Geography and subdivisions Kildare is the 24th-largest of Ireland's 32 counties in area and the seventh largest in terms of population. It is the eighth largest of Leinster's twelve counties in size, and the second largest in terms of population. It is bordered by the counties of Carlow, Laois, Meath, Offaly, South Dublin and Wicklow. As an inland county, Kildare is generally a lowland region. The county's highest points are the foothills of the Wicklow Mountains bordering to the east. The highest point in Kildare is Cupidstown Hill on the border with South Dublin, with the better known Hill of Allen in central Kildare. Towns and villages * Allen * Allenwood * Ardclough * Athy * Ballitore * Ball ...
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Lullymore
Lullymore () is a civil parish in County Kildare in Ireland. It is in the historical barony of Offaly East. The lowest observed 20th century air temperature in Ireland, -18.8 °C was measured at Lullymore on 2 January 1979. Location Lullymore is situated on the R414 between Rathangan and Allenwood. The village forms an island of arable land, surrounded on all sides by the Bog of Allen. Lullymore is situated 6 miles from Rathangan and approx 3 miles from Allenwood. Business Lullymore briquette factory, operated by Bord Na Mona opened in 1936 and closed in 1992 due to falling demand for its products. Sport and amenities Lullymore Heritage & Discovery Park is a visitor attractions in the Kildare region. It is a destination for families, school tours, birthday parties and tourists. The Bog of Allen Nature Centre, run by Irish Peatland Conservation Council The Irish Peatland Conservation Council (IPCC; ) is a national charitable organisation established in 1982 to conser ...
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Rivers Of Ireland
Shown here are all the major rivers and tributaries of Ireland with their lengths (in kilometres and miles). Starting with the Northern Ireland rivers, and going in a clockwise direction, the rivers (and tributaries) are listed in regard to their entry into the different seas: the Irish Sea, the Celtic Sea and the Atlantic Ocean. Also shown are two tables. ''Table 1'' shows the longest rivers in Ireland with their lengths (in kilometres and miles), the counties they flow through, and their catchment areas (in square kilometres). ''Table 2'' shows the largest rivers in Ireland (by mean flow) in cubic metres per second. The longest river in Ireland is the River Shannon, at . The river develops into three lakes along its course, Lough Allen, Lough Ree and Lough Derg. Of these, Lough Derg is the largest. The Shannon enters the Atlantic Ocean at the Shannon Estuary. Other major rivers include the River Liffey, River Lee, River Swilly, River Foyle, River Lagan, River Erne, River Bla ...
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Brown Trout
The brown trout (''Salmo trutta'') is a European species of salmonid fish that has been widely introduced into suitable environments globally. It includes purely freshwater populations, referred to as the riverine ecotype, ''Salmo trutta'' morpha ''fario'', a lacustrine ecotype, ''S. trutta'' morpha ''lacustris'', also called the lake trout, and anadromous forms known as the sea trout, ''S. trutta'' morpha ''trutta''. The latter migrates to the oceans for much of its life and returns to fresh water only to spawn. Sea trout in Ireland and Britain have many regional names: sewin in Wales, finnock in Scotland, peal in the West Country, mort in North West England, and white trout in Ireland. The lacustrine morph of brown trout is most usually potamodromous, migrating from lakes into rivers or streams to spawn, although evidence indicates some stocks spawn on wind-swept shorelines of lakes. ''S. trutta'' morpha ''fario'' forms stream-resident populations, typically in alpine stre ...
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European Perch
The European perch (''Perca fluviatilis''), also known as the common perch, redfin perch, big-scaled redfin, English perch, Euro perch, Eurasian perch, Eurasian river perch, Hatch, poor man’s rockfish or in Anglophone parts of Europe, simply the perch, is a predatory species of the freshwater perch native to Europe and northern Asia. The species is a popular quarry for anglers, and has been widely introduced beyond its native area, into Australia, New Zealand and South Africa. They have caused substantial damage to native fish populations in Australia and have been proclaimed a noxious species in New South Wales. Description European perch are greenish with red pelvic, anal and caudal fins. They have five to eight dark vertical bars on their sides. When the perch grows larger, a hump grows between its head and dorsal fin. European perch can vary greatly in size between bodies of water. They can live for up to 22 years, and older perch are often much larger than average; t ...
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Northern Pike
The northern pike (''Esox lucius'') is a species of carnivorous fish of the genus '' Esox'' (the pikes). They are typical of brackish and fresh waters of the Northern Hemisphere (''i.e.'' holarctic in distribution). They are known simply as a pike in Britain, Ireland, and most of Eastern Europe, Canada and the United States. Pike can grow to a relatively large size: the average length is about , with maximum recorded lengths of up to and published weights of . The IGFA currently recognizes a pike caught by Lothar Louis on Greffern Lake, Germany, on 16 October 1986, as the all-tackle world-record northern pike. Northern pike grow to larger sizes in Eurasia than in North America, and typically grow to larger sizes in coastal than inland regions of Eurasia. Etymology The northern pike gets its common name from its resemblance to the pole-weapon known as the pike (from the Middle English for 'pointed'). Various other unofficial trivial names are common pike, Lakes pike, great n ...
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Slate River Mouth
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for exam ...
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Slate River Source
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcano, volcanic ash (volcanic), ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility (geology), fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety o ...
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