Marble Arch Caves
http://dbpedia.org/resource/Marble_Arch_Caves an entity of type: Thing
Marble Arch leizeak Ipar Irlandako hego-mendebaldean dagoen Fermanagheko konderriko leize famatuak dira. Florencecourt herrixkaren ondoan daude, Irlandako Errepublikarekiko mugatik hurbil.
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The Marble Arch Caves are a series of natural limestone caves located near the village of Florencecourt in County Fermanagh, Northern Ireland. The caves are named after the nearby Marble Arch, a natural limestone arch at the upstream end of Cladagh Glen under which the Cladagh River flows.The caves are formed from three rivers draining off the northern slopes of Cuilcagh mountain, which combine underground to form the Cladagh. On the surface, the river emerges from the largest karst resurgence in Ireland, and one of the largest in the United Kingdom.At 11.5 kilometres (7.1 mi) the Marble Arch Caves form the longest known cave system in Northern Ireland, and the karst is considered to be among the finest in the British Isles.
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Die Marble Arch Caves (irisch Uaimheanna na hÁirse Marmair, dt. Marmorbogenhöhlen) liegen im Kalksteinareal des County Fermanagh bei in Nordirland. Das südwestliche Gebiet ist für die und für das Sandsteinplateau der Cuilcagh Mountain bekannt, das die Landschaft bis auf etwa 670 m über NN anhebt.
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Marble Arch Caves
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Marble Arch leizeak
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Marble Arch Caves
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Marble Arch Caves
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Marble Arch Caves
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Marble Arch Cave
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Aghinrawn River sink
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Owenbrean River sink
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Sruh Croppa River sink
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The main section of Marble Arch Cave is fed by three rivers on the slopes of Cuilcagh Mountain.
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94 m
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Marble Arch Cave
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Aghinrawn River sink
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Owenbrean River sink
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Sruh Croppa River sink
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blue
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top
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near Florencecourt,
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Blue pog.svg
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Uaimheanna an hÁirse Marmair
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Marble Arch Caves - gour pools and flowstone.jpg
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("The Castle" gour pool formations in the Marble Arch Caves show cave.)
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Die Marble Arch Caves (irisch Uaimheanna na hÁirse Marmair, dt. Marmorbogenhöhlen) liegen im Kalksteinareal des County Fermanagh bei in Nordirland. Das südwestliche Gebiet ist für die und für das Sandsteinplateau der Cuilcagh Mountain bekannt, das die Landschaft bis auf etwa 670 m über NN anhebt. Das Wetter wird vom nur 56 km entfernten Atlantik beeinflusst. Im Moorland der Cuilcagh Mountain dringt der Regen in den Torf ein und erreicht nur sehr verzögert die Flüsse. Während des Sommers sind die Flüsse wasserarm, aber nach schwerem Niederschlag strömt eine große Menge Wasser die Hänge herab, wo der Torf den darunter liegenden Sandstein bedeckt. Sie laufen von dort in die unterirdischen Gänge der Marble Arch Caves, die seit 1895 erforscht werden und 2004 zum europäischen Geopark erklärt wurden. Ein Teil der Höhlen wird mit Booten befahren.
* Marble Arch Caves
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Marble Arch leizeak Ipar Irlandako hego-mendebaldean dagoen Fermanagheko konderriko leize famatuak dira. Florencecourt herrixkaren ondoan daude, Irlandako Errepublikarekiko mugatik hurbil.
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The Marble Arch Caves are a series of natural limestone caves located near the village of Florencecourt in County Fermanagh, Northern Ireland. The caves are named after the nearby Marble Arch, a natural limestone arch at the upstream end of Cladagh Glen under which the Cladagh River flows.The caves are formed from three rivers draining off the northern slopes of Cuilcagh mountain, which combine underground to form the Cladagh. On the surface, the river emerges from the largest karst resurgence in Ireland, and one of the largest in the United Kingdom.At 11.5 kilometres (7.1 mi) the Marble Arch Caves form the longest known cave system in Northern Ireland, and the karst is considered to be among the finest in the British Isles.
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Show cave; accessible beyond with permission from Marble Arch Caves centre
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1895
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Location of main entrance to Marble Arch Cave.
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Point at which the Sruh Croppa River goes underground. NB: In dry weather, the river sinks upstream of this point.
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Point at which the Owenbrean River goes underground, at a cave named Pollasumera. Some of the river flow also sinks further upstream of this point.
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Point at which the Aghinrawn River goes underground, at the base of Monastir Cliff.
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Gour pool, or rimstone, calcite formations.
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