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48-464: Corrib has multiple meanings. Among the possible ones are: Lough Corrib , a lake in the west of Ireland, north of Galway. River Corrib , a river connecting Lough Corrib to Galway Bay through the city of Galway. Corrib gas field , a natural gas reservoir in the Atlantic, about 80 km off County Mayo on the west coast of Ireland Topics referred to by

96-587: A Special Area of Conservation . Loch Coirib is a corruption of Loch Oirbsean . According to placename lore, this refers to Oirbsen or Oirbsiu—another name for the Tuatha Dé Danann figure Manannán mac Lir —who is believed to have been a god of the sea. In Irish, the lough is also called An Choirib ("the Corrib"). Surveys have been undertaken since 2007 by a local surveyor/cartographer to create up-to-date charts of Lough Corrib. These have uncovered

144-430: A number of transitional and intermediate bogs , which in different ways combine characteristics of both raised bogs and fens. (See bog .) The main constituents of the peat are rootless peat mosses that grow slowly in height whilst at the same time the lower layer becomes peat as the air is excluded. Depending on the geographical location, various species of peat moss are involved in making a raised bog. The growth rate of

192-558: A number of objects of historical significance, which have been investigated by the Underwater Archaeology Unit of the National Monuments Service . These include Bronze Age and Iron Age vessels ( dugout canoes ), the "Annaghkeen Boat" being 40 ft in length and intricately carved, the "Carrowmoreknock Boat", a well preserved 10th century vessel carrying three Viking battle axes , and

240-542: A result of freeze-thaw processes of the surrounding water. The low temperatures prevent full decomposition of the organic material. Polygonal bogs ( Polygonmoore ) are widespread on the Arctic and sub-Arctic plains of Siberia and North America and cover vast areas. They are associated with patterned peatland and ice wedges . A scanty layer of peat-forming vegetation can occur in the inner honeycomb-shaped areas of this frost pattern terrain ( cryoturbation ) and are fed during

288-434: A secondary process after the silting up of lakes or oxbows (see illustration on the right in the sequence). At first, fens emerged under the influence of groundwater ( minerotrophy ). Oxygen deficiencies and high acidity in the constantly moist substrate inhibited the decomposition of dead plant parts and led to peat formation. Thus the raised bog rises very slowly above the groundwater level, hence its name. As

336-525: Is Caislean-na-Circe, between Maam and Doon. This section of Lough Corrib is free from islands except for the rock on which the ancient Hen's Castle of the O'Connor's and the O'Flaherty's stands. The castle was home of the pirate Queen Gráinne O'Malley , who lived in the time of Queen Elizabeth I of England . In 1225, the Lord Justice caused Odo O'Flatherty to give up Kirk Castle to Odo O'Connor, King of Connaught; for assurance of his fidelity. Cruises on

384-464: Is a succession of raised bog types along the line of descent towards the ocean, from northwest to southeast. As a result of peat use, raised bogs have been harvested for peat and cultivated, apart from a few remnants (less than 10% of the original area). The largest contiguous raised bog in central Europe was the Bourtange Moor , which originally covered an area of about 2,300 km including

432-462: Is counted as a geological subsoil due to the small earth-forming processes that are still going on and is known as the peat preservation horizon ( Torferhaltungshorizont ). In raised bogs, the upper peat layer is called white peat, since it consists of largely undecomposed light brown peat mosses. The lower layer is black peat, which is already well humified and has a black-brown colour with still recognizable plant remains. The formation of raised bogs

480-616: Is dependent on the climate, that is to say the amount of precipitation and rate of evaporation, which in turn are decisively determined by the temperature. In addition, the relief of the terrain has an influence on the water discharge behaviour and thus the shape of a raised bog. This results in geographical limitations to the formation of raised bogs. Favourable conditions for the development of raised bogs are found mainly in North America ( Canada and Alaska ), Northern Europe and Western Siberia , South America , Southeast Asia and in

528-411: Is destroying fish habitat and the zebra mussel . On 21 March 2007, Cryptosporidium was confirmed to be present in the drinking water of Galway City , Moycullen , Oughterard and Headford , which had been instructed six days earlier to boil their water before drinking. The water taken from Lough Corrib was likely contaminated by migration of animal and human faeces . Controversy emerged when it

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576-473: Is different from Wikidata All article disambiguation pages All disambiguation pages Lough Corrib Lough Corrib ( / l ɒ x ˈ k ɒr ɪ b / lokh KORR -ib ; Irish : Loch Coirib ) is a lake in the west of Ireland. The River Corrib or Galway River connects the lake to the sea at Galway . It is the largest lake within the Republic of Ireland and the second largest on

624-512: Is not yet clear how these bogs have emerged as mosses are entirely absent here. Coastal bogs ( Planregenmoore ) or Atlantic bogs, as their names suggest, tend to form close to the sea. In addition, in regions covered by blanket bog, there are also lightly convex coastal bogs with low energy surface relief in level locations. The distribution of coastal bogs in Europe extends from Ireland to the east via South Norway to Southwest Sweden and north to

672-428: Is strongly decomposed, and an overlying white peat layer which is less decomposed. This difference is a result of changes in the hydrology of the bog. The white peat grew more rapidly under humid conditions than the black peat. This is attributed to a climate change with high precipitation and low evaporation around 1000 to 500 BC. As a result, the peat moss growth grew locally and the black peat/white peat boundary layer

720-634: The Amazon Basin . In these regions, bogs of all kinds and peat deposits of four million square kilometres have been formed, covering three percent of the Earth's surface. In the southern hemisphere low-mineral-rich bogs are rarely formed from peat mosses. Only in the Tierra del Fuego do peat moss raised bogs exist. The most peaty countries in the tropics are found in Southeast Asia. In many cases it

768-599: The Annex 1 habitats : active raised bog, turlough (both priority habitats), degraded raised bog (capable of regeneration) and vegetation of depressions (rhynchosporion). These habitats are considered to be among the best examples in Ireland due to their relatively large size and the generally low levels of disturbance. In the Natura form compiled for the site active raised bog was given a rating of A (Excellent value) which emphasises

816-637: The Black Forest the Wildseemoor has been protected and, in the Vosges on le Tanet , north of the Col de la Schlucht a large area has been protected. The Alpine Foreland , which was formed by ice-age glaciation, is also rich in peatland. The Wurzacher Ried (Haidgauer Regenmoorschild) is considered the largest and best preserved raised bog in central Europe. Other raised bogs and peatland areas include

864-734: The Federsee , the High Fens on the Germano-Belgian border, the Ewiges Meer near Aurich and the Lengener Meer near Wiesmoor. In 2003, Estonia exported 3.6 million m³ of peat for west European garden use, more than 60% of the state production. In Lithuania 60% of the usable peat area has been prepared for extraction or is already exhausted. Lough Lurgeen Bog and Glenamaddy Turlough Bog contains very good examples of

912-590: The Lofoten . In North America there are coastal bogs in the area of the Great Lakes (especially in Minnesota and Ontario ). Coastal bogs are also fed exclusively by rain. In the less oceanically influenced climatic regions of North-West Europe (lower precipitation), raised bogs take on the classical lens shape and are called plateau bogs or plateau raised bogs ( Plateauregenmoore ). They grow more strongly in

960-594: The island of Ireland (after Lough Neagh ). It covers 176 km² and lies mostly in County Galway with a small area of its northeast corner in County Mayo . The first canal on the island of Ireland was cut in the 12th century. Known as the Friar's Cut, it allowed boats to pass from Lough Corrib to the sea at Galway. Lough Corrib was designated a Ramsar site on 16 June 1996. It has also been designated

1008-957: The Dutch portion, but only small sections remain. The largest remaining raised bog in northern Europe is the 76 km Lille Vildmose . Other large raised bogs are the Teufelsmoor northeast of Bremen, the Vehnemoor (exhausted) and the Esterweger Dose (formerly about 80 km , exhausted) between Oldenburg and Papenburg. The raised bogs of the Central Uplands of the Harz , Solling , Thuringian Forest ( Großer Beerberg , Schneekopf - Teufelsbad, Fichtenkopf, Saukopf), Giant Mountains , Ore Mountains , Fichtel and Rhön ( Black Moor , Red Moor ) are, by contrast, comparatively small. In

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1056-474: The Scandinavian hills, central Finland, Karelia and north Siberia. In North America, Alaska is the main location for string bogs, thanks to its cold continental climate. Frost action plays an important role in these bogs. On the ridges or hummocks, ground ice is found until early summer. Palsa bogs ( Palsamoore or Palsenmoore ) are found on the margins of the Arctic permafrost soils ( tundra ). Here

1104-476: The central area of these bogs, there are always large kolks. In northern Russia and western Siberia, kermis frequently occur in giant complexes where the bogs have grown into one another. Kermis are also found in Finland in the central and northern boreal forest zone. String bogs or aapa fens ( Aapamoore or Strangmoore ) are typically found on the northern fringes of the distribution area for raised bogs, in

1152-433: The centre than at the margins. This results in the centre of the bog bulging, hence the name "raised bog". This bulging can be several metres high. As a result, the perimeter of the bog is more or less inclined, and is known as the rand . The sloping bog sides of larger bogs are traversed by drainage channels or soaks ( Rüllen ) through which excess water is discharged. Other characteristic structures of these raised bogs are

1200-429: The entire system is very important from both a hydrological and ecological perspective. A region of peatland extends from Alaska in the west to the coast of the Atlantic in the east, and is comparable in size to that of West Siberia. A zone of domed raised bogs adjoins the zones of palsa bogs and string fens. In the direction of descent towards the ocean, blanket bogs occur east of Hudson Bay. These are superseded towards

1248-562: The fact that this type of bog rises in height over time as a result of peat formation. They are like sponges of peat moss, full of water, that form a more or less dome shape in the landscape. In Germany, the term Hochmoor ( lit.   ' high bog ' ) strictly refers only to the classical, lens-shaped bogs of northwest Germany . The bogs are not influenced by mineral-rich groundwater or surface water, but are fed exclusively by precipitation — mainly rainwater, hence their alternative German designation of Regenmoor or "rain-fed bog". Thus

1296-571: The flat, treeless raised bog core with its characteristic microrelief of shallow wet depressions or flarks ( Schlenken ) alternating with hummocks ( Bülten ) of drier peat moss. Larger accumulations of water in the middle of the bogs are called kolks or bog ponds (of humic acid -rich water); the wet area on the outer margins is known as a moat or lagg . Genuine ombrotrophic bogs on the North German Plain are usually sharply divided into two layers: an underlying black peat layer, which

1344-458: The importance of the site. Raised bog habitats are now very rare in Europe and it has recently been estimated that the Republic of Ireland contains 50% of the relatively intact oceanic raised bog systems in Europe. The site contains the second largest area of intact raised bog surface in Ireland. The combination of raised bog, oligotrophic lake and turlough habitats is unique in Ireland and thus

1392-465: The inspiration" for The Hounds of the Morrigan , a children's novel by Pat O'Shea . See Annals of Inisfallen (AI) Raised bog Raised bogs are very threatened by peat cutting and pollution by mineral salts from the surrounding land (due to agriculture and industry ). The last great raised bog regions are found in western Siberia and Canada . The term raised bog derives from

1440-496: The island. There is evidence of an early monastic settlement, and two churches - Saint Patrick 's and the 12th century church known as the "saints" church. St. Brendan of Clonfert is also said to have spent some time on an island in this lake after returning from his travels in Britain. There are several paths around the island, an old cemetery and remains of four or five cottages which housed the few inhabitants. Another lake island

1488-501: The kermi bog type. They represent probably the most important type of raised bog on earth. The Vasyugan Swamp in this region, is the largest bog system on earth and covers more than 50,000 km (19,000 sq mi). It is estimated to contain over 14 billion tonnes of peat deposits. The largest central European raised bog areas are the southern North Sea coastal area and the Alpine Foreland . As in North America there

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1536-608: The lake, e.g. woodland, callows grassland and raised bog , have been incorporated into the Special Area of Conservation. In early 2007, large numbers of the protozoan parasite Cryptosporidium were detected in water from the lake, leading to contamination of the public water supply in Galway city and an outbreak of cryptosporidiosis . Another unwelcome visitor is the invasive species Lagarosiphon major (also known as 'curly-leaved waterweed' or 'South African pondweed') which

1584-402: The latter refers to all bogs, not just those that are arched or only slightly arched, but which nevertheless are characterized by an extreme mineral salt deficiency and other resulting ecological properties. A living raised bog needs a moist, balanced climate in which to grow. The quantity of precipitation has to be greater than the water losses through discharge and evaporation. In addition,

1632-453: The left in the sequence). They are formed either as a primary bog due to the erosion of previously dry mineral soils, for example due to clearing, climate change or infiltration, or as a secondary process as a result of the growth of a raised bog on neighbouring mineral soil. The formation of a typical raised bog is a very slow process, which lasts from centuries to a thousand years even in favourable, undisturbed conditions. Furthermore, there are

1680-463: The lough depart from Cong , Ashford Castle, Galway City, and Oughterard. Paul Féval 's novel La Quittance de minuit (1846) is set in County Galway , near Lough Corrib. William Wilde , father of Oscar Wilde , wrote a book about the lake, Lough Corrib, its Shores and Islands (1867). He built a summerhouse on the banks of the lake, called Moytura House. The Irish Times states that "the unspoilt countryside around Lough Corrib provided

1728-477: The margins of lowland bogs i.e. fens , or transition into them. Kermi bogs ( Kermimoore, Schildhochmoore, Strangmoore or Blankenmoore ) or kermi raised bogs have only a slightly domed shape. The surface of the bog rises steadily from the broad lagg zone. Kermis have ridge-shaped hummocks of peat moss, that are aligned with the contours of the bog. The flarks or elongated depressions are generally tub-shaped and hardly distinguishable externally from kolks . In

1776-460: The peat layer is only about a millimetre per year. Growing bogs can be divided into two layers. The ' acrotelm ' ( Greek : akros = highest; telma = bog) is the upper part and includes the vegetation layer and the bog 'floor'. Here fresh organic substances (peat formation horizon) are created by the growth and dying of plant elements. The "catotelm" (Greek: kato = below) is the underlying water-saturated part with less biological activity. This layer

1824-484: The precipitation must be evenly spread through the year. Raised bogs in Europe have been developing for about 11,000 years, since the beginning of the Holocene and after the retreat of the last ice sheet . As far as their origins are concerned, a distinction is made between lake mires or 'siltation-formed raised bogs' ( Verlandungshochmoore ) and 'mire-formed raised bogs' ( wurzelechte Hochmoore ). The former emerged in

1872-412: The resulting peat slowly rises above the influence of mineral salts in the groundwater, it reaches a point where the development of the raised bog begins to change in nature; that is, the bog now becomes fed solely by rainwater, which is low in salt. By contrast, mire-formed raised bogs are created directly on the mineral substrate of low-salt areas without having been initially formed as fens (see figure on

1920-478: The ridges of the string bogs can grow into hummocks several metres high. Like string bogs, the so-called palsas frequently lie within peatlands fed by mineral soil water. Some are surrounded by water-filled, ditch-like hollows. Peat formation is limited; these bogs are peat deposits from warmer, interglacial periods and did not experience frost heaving of their inner core of ice until the climate became colder. These ice lenses increase in size from year to year as

1968-408: The same term [REDACTED] This disambiguation page lists articles associated with the title Corrib . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Corrib&oldid=542589503 " Category : Disambiguation pages Hidden categories: Short description

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2016-400: The short summers with sufficient moisture, because the meltwater is prevented from draining away by the raised polygonal margins. The peat layers can attain a thickness of 0.3 to 1 m (1.0–3.3 ft). The west Siberian raised bog area covers 700,000 km (270,000 sq mi). The large bogs have domes in the centre up to 10 m (33 ft) high. They are predominantly of

2064-413: The south and a larger deeper basin to the north. These two parts are connected by a narrow channel. In the southern and eastern parts of the lake, the lake bed is dominated by limestone bedrock covered by deposits of precipitated marl. The surrounding land is mostly pastoral farmland to the south and east and bog to the west and north. In addition to the lake basis, some areas of scientific interest adjoining

2112-503: The sub-polar zone, north of the 66th latitude in the northern hemisphere. Here, raised bogs only occur as islands within wetlands supplied by mineral soil water. On level ground these islands are irregularly distributed; on hillsides they form ridges parallel to the contours and at right angles to line of slope. The ridges separate boggy hollows of mineral soil known by the Finnish word, rimpis . The main distribution area for string bogs are

2160-554: The wreck of a Victorian pleasure yacht. The lake is hence of international importance as a marine archaeological site. All historic wrecks in the lough are protected, and a licence to dive them is required from the National Monuments Service. The wildlife in Lough Corrib includes birds and hawks, otters, mink, stoat, frogs, and bats. Lough Corrib can be divided into two parts: a smaller shallower basin to

2208-572: Was formed in April 2007 to highlight the issue. While Lough Corrib is reputed to have 365 islands, a recent figure from the creator of the charts of the lake is 1,327. These islands include Inchagoil Island, midway between Cong and Oughterard . It is one of the largest of the wooded islands along Lough Corrib. The island has views of the Maumturk range, Joyce Country and the mountains of Connemara . There are some beaches and woods with walks around

2256-427: Was formed, although this did not develop simultaneously in all raised bogs. Raised bogs also occur in precipitation-rich upland regions at the montane and, more rarely, alpine levels (i.e. above the tree line ). As a result of the sloping terrain, they often have a characteristic, asymmetric or non-concentric appearance. Mountain or upland bogs may be topographically divided into: All these bog types may occur on

2304-711: Was revealed that funds previously earmarked to improve Galway's water system had not been spent. Dick Roche , the Minister of the Environment, later announced allocation of additional funds to tackle the issue. Measures included upgrading existing water treatment and filtration systems, as well as the projected importing of water from nearby Luimnagh, Tuam , County Galway. This plant at Luimnagh has facilities for Cryptosporidium eradication and filtration. The Community Care Organisation, Cope, delivered bottled water to their elderly clients from 30 March 2007. A lobby group

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