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Killarney National Park
Killarney National Park ( ga, Páirc Náisiúnta Chill Airne), near the town of Killarney, County Kerry, was the first national park in Ireland, created when the Muckross Estate was donated to the Irish Free State in 1932. The park has since been substantially expanded and encompasses over 102.89 km2 (25,425 acres) of diverse ecology, including the Lakes of Killarney, oak and yew woodlands of international importance, and mountain peaks. It has the only red deer herd on mainland Ireland and the most extensive covering of native forest remaining in Ireland. The park is of high ecological value because of the quality, diversity, and extensiveness of many of its habitats and the wide variety of species that they accommodate, some of which are rare. The park was designated a UNESCO Biosphere Reserve in 1981. The park forms part of a Special Area of Conservation and a Special Protection Area. The National Parks and Wildlife Service is responsible for the management and adm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Killarney
Killarney ( ; ga, Cill Airne , meaning 'church of sloes') is a town in County Kerry, southwestern Ireland. The town is on the northeastern shore of Lough Leane, part of Killarney National Park, and is home to St Mary's Cathedral, Ross Castle, Muckross House and Abbey, the Lakes of Killarney, MacGillycuddy's Reeks, Purple Mountain, Mangerton Mountain, Paps Mountain, the Gap of Dunloe and Torc Waterfall. Its natural heritage, history and location on the Ring of Kerry make Killarney a popular tourist destination. Killarney won the Best Kept Town award in 2007, in a cross-border competition jointly organised by the Department of the Environment and the Northern Ireland Amenity Council. In 2011, it was named Ireland's tidiest town and the cleanest town in the country by Irish Business Against Litter. History Early history and development Killarney featured prominently in early Irish history, with religious settlements playing an important part of its recorded history. Its fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Special Protection Area
A Special Protection Area (SPA) is a designation under the European Union Directive on the Conservation of Wild Birds. Under the Directive, Member States of the European Union (EU) have a duty to safeguard the habitats of migratory birds and certain particularly threatened birds. Together with Special Areas of Conservation (SACs), the SPAs form a network of protected sites across the EU, called Natura 2000. Each SPA has an EU code – for example the North Norfolk Coast SPA has the code ''UK9009031''. In the United Kingdom As at 21 September 2006, there were 252 classified SPAs and 12 proposed SPAs in England, Scotland, Wales and Northern Ireland. The Conservation (Natural Habitats etc.) Regulations 1994 implement the terms of the Directive in Scotland, England and Wales. In Great Britain, SPAs (and SACs) designated on land or in the intertidal area are normally also notified as Sites of Special Scientific Interest (SSSIs), and in Northern Ireland as Areas of Special Scientific ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Innisfallen
Innisfallen ( ) or Inishfallen (from ga, Inis Faithlinn , meaning 'Faithlinn's island') is an island in Lough Leane; one of the three Lakes of Killarney in County Kerry, Ireland. Innisfallen is home to the ruins of Innisfallen Abbey. Geography Innisfallen is situated about the midway in Lough Leane, County Kerry. The island is some in area, mostly wooded, with undulating hills and many slopes. It lies within the Killarney National Park. Access It is possible for tourists to visit the island during the summer months, with boats leaving from Ross Castle throughout the day. History Innisfallen is home to the ruins of Innisfallen Abbey, one of the most impressive archaeological remains dating from the early Christian period. The monastery was founded in 640 by Saint Finian and was occupied for approximately 950 years. Over a period of about 300 of these, the monks wrote the Annals of Innisfallen, which chronicle the early history of Ireland as it was known to the monks. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lough Leane
Lough Leane (; ) is the largest of the three lakes of Killarney, in County Kerry. The River Laune flows from the lake into the Dingle Bay to the northwest. Etymology and history The lake's name means "lake of learning" probably in reference to the monastery on Innisfallen, an island in the lake. Innisfallen was a centre of scholarship in the early Middle Ages, producing the ''Annals of Innisfallen'' and, according to legend, educating King Brian Boru. Another historic site, the tower house Ross Castle sits on Ross Island in the lake. Ross Island is rich in copper. Archaeological evidence suggests the island has been mined since the time of the Bronze Age Beaker People.J. P. N. Northover, W. O'Brien and S. Stos. "Lead Isotopes and Metal Circulation In Beaker/Early Bronze Age Ireland." ''The Journal of Irish Archaeology'' Vol. 10, (2001), pp. 25-47. Wordwell Ltd. Stable URL: https://www.jstor.org/stable/30001669 Geography Lough Leane is approximately in size. It is also the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Pavement
A limestone pavement is a natural karst landform consisting of a flat, incised surface of exposed limestone that resembles an artificial pavement. The term is mainly used in the UK and Ireland, where many of these landforms have developed distinctive surface patterning resembling paving blocks. Similar landforms in other parts of the world are known as alvars. Formation of a limestone pavement Conditions for limestone pavements are created when an advancing glacier scrapes away overburden and exposes horizontally bedded limestone, with subsequent glacial retreat leaving behind a flat, bare surface. Limestone is slightly soluble in water and especially in acid rain, so corrosive drainage along joints and cracks in the limestone can produce slabs called ''clints'' isolated by deep fissures called ''grikes'' or ''grykes'' (terms derived from a northern English dialect). If the grykes are fairly straight and the clints are uniform in size, the resemblance to man-made paving stone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Limestone
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup. Depositional basins Within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east–west aligned belt of land stretching through central Wales and the English Midlands to East Anglia and on into Belgium. The limestones deposited to its south form a distinct South Wales-Mendip province which extends from Pembrokeshire in the west through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Red Sandstone
The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the ancient continent of Euramerica, Euramerica/Laurussia. In Britain it is a lithostratigraphy, lithostratigraphic unit (a sequence of rock strata) to which Stratigraphy, stratigraphers accord Geological unit#Lithostratigraphic units, supergroup status and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain. Sedimentology The Old Red Sandstone describes a suite of sedimentary rocks deposited in a variety of environments during the Devonian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Purple Mountain (Kerry)
Purple Mountain () at high, is the 21st–highest peak in Ireland on the Arderin scale, and the 28th–highest according to the Vandeleur-Lynam scale. It is located in County Kerry, and is the highest point of the Purple Mountain Group. Geology Purple Mountain is composed of sandstone particles of various sizes which are collectively known as ''Old Red Sandstone''. Old Red Sandstone has a purple-reddish colour, and has virtually no fossils. The colour gave its name to the mountain group. The composition of ''Old Red Sandstone'' is variable and contains quartz stones, mudstones, siltstones, and sandstone particles (boulders of conglomerate rock containing quartz pebbles are visible). Geography The Purple Mountain Group is described as a "heather–strewn" massif with five classified peaks at its centre: Purple Mountain , Purple Mountain NE Top and Shehy Mountain , Tomies Mountain (also called An Chathair) , and Tomies North Top (also called Tomies Rock, or Tomies Chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shehy Mountains
The Shehy Mountains (''Cnoic na Seithe'' in Irish language, Irish, meaning ''"Hills of the animal hides"'') are a range of low mountains situated on the border between County Cork and County Kerry, in Republic of Ireland, Ireland. Geography and geology The highest peak (also the highest mountain in County Cork), Knockboy (''Cnoc Buí'', "yellow hill"), is 706 metres high and most of the other peaks in the range are between 500 and 600 metres high. The River Lee (Ireland), River Lee rises in Coomroe, a small valley at the eastern end of the range, before flowing eastwards towards Cork Harbour, where it enters the sea. The peaks mostly consist of Old Red Sandstone laid down in the Devonian period. During the Last Glacial Period, Ice Age, the Shehys took their present form, when glaciers carved out the many deep valleys in the area and also eroded the mountains down to their present height. When the icecaps retreated, they left behind hundreds of lakes in the valleys and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torc Mountain
Torc Mountain (), at , is the 329th–highest peak in Ireland on the Arderin list. It is a popular mountain for hill walkers as it has a stone or boarded path (using railway sleepers) from its base at Torc Waterfall to its summit, which has views of the Lakes of Killarney. Torc Mountain is part of the Mangerton Mountain Group range in County Kerry, Ireland. Naming The word Torc comes from the Irish translation of a "wild boar", and the area is associated with legends involving wild boars – Irish academic Paul Tempan notes that: "Wild boar is significant in Celtic mythology, being depicted on Celtic artefacts found in continental Europe, Ireland and Britain; it represents physical strength and heroic fighting skills". One legend is of a man who was cursed by the Devil to spend each night transformed into a wild boar, but when his secret was revealed by a local farmer, he burst into flames and disappeared into the nearby '' Devil's Punchbowl'' on Mangerton Mountain from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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