Ardgroom Gaelic Footballers
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Ardgroom Gaelic Footballers
Ardgroom () is a village on the Beara peninsula in County Cork, Ireland. Its name refers to two gravelly hills deposited by a glacier, Dromárd and Drombeg. It lies to the north north west of Glenbeg Lough, overlooking the Kenmare River estuary. It sits between the coast and the Slieve Miskish Mountains. The village contains a shop, post office, a petrol station and "The Village Inn" pub. Stone circle Near the village lie a number of megalithic monuments. Signposted is the stone circle to be found to the east of the village at a distance of about 1 mile, off the old Kenmare road. It has the name "Canfea" but is normally called the "Ardgroom" stone circle. About 1 mile north east lie the remains of another stone circle. The circle consists of 11 stones, 9 of which are still upright with one alignment stone outside the circle. Unusually for a stone circle, its stones tend to taper toward points. Also in the vicinity are the remains of at least two ring fort Ringforts, ri ...
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Republic Of Ireland
Ireland ( ga, Éire ), also known as the Republic of Ireland (), is a country in north-western Europe consisting of 26 of the 32 counties of the island of Ireland. The capital and largest city is Dublin, on the eastern side of the island. Around 2.1 million of the country's population of 5.13 million people resides in the Greater Dublin Area. The sovereign state shares its only land border with Northern Ireland, which is part of the United Kingdom. It is otherwise surrounded by the Atlantic Ocean, with the Celtic Sea to the south, St George's Channel to the south-east, and the Irish Sea to the east. It is a unitary, parliamentary republic. The legislature, the , consists of a lower house, ; an upper house, ; and an elected President () who serves as the largely ceremonial head of state, but with some important powers and duties. The head of government is the (Prime Minister, literally 'Chief', a title not used in English), who is elected by the Dáil and appointed by ...
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Glenbeg Lough
Glenbeg Lough is a freshwater lake in the southwest of Ireland. It is located on the Beara Peninsula in County Cork. Geography Glenbeg Lough measures about long and wide. It lies about southwest of Kenmare, near the village of Ardgroom. Hydrology Glenbeg Lough drains into the Ownagappul River, which in turn enters Kenmare Bay at Cappul. The lake is oligotrophic. Natural history Fish species in Glenbeg Lough include brown trout, salmon and the critically endangered European eel. The lake is part of the Glanmore Bog Special Area of Conservation. See also *List of loughs in Ireland References {{Reflist, refs = {{Google maps , url = https://www.google.com/maps/place/Glenbeg+Lough,+Co.+Cork,+Ireland/@51.7154702,-9.8804428,15z/data=!3m1!4b1!4m2!3m1!1s0x48457c73ab0aa2e9:0x7e05c3c9cce4351a?hl=en , title = Glenbeg Lough , access-date = 4 January 2016 {{cite report , last1 = Free , first1 = Gary , last2 = Little , first2 = Ruth , last3 = Tierney , first3 = Deirdre , last4 ...
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Stone Circles In Ireland
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. M ...
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Ring Fort
Ringforts, ring forts or ring fortresses are circular fortified settlements that were mostly built during the Bronze Age up to about the year 1000. They are found in Northern Europe, especially in Ireland. There are also many in South Wales and in Cornwall, where they are called rounds. Ringforts come in many sizes and may be made of stone or earth. Earthen ringforts would have been marked by a circular rampart (a bank and ditch), often with a stakewall. Both stone and earthen ringforts would generally have had at least one building inside. Distribution Ireland In Irish language sources they are known by a number of names: ' (anglicised ''rath'', also Welsh ''rath''), ' (anglicised ''lis''; cognate with Cornish '), ' (anglicised ''cashel''), ' (anglicised ''caher'' or ''cahir''; cognate with Welsh ', Cornish and Breton ') and ' (anglicised ''dun'' or ''doon''; cognate with Welsh and Cornish ').Edwards, Nancy. ''The Archaeology of Early Medieval Ireland''. Routledge, 20 ...
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Stone Circle
A stone circle is a ring of standing stones. Most are found in Northwestern Europe – especially in Britain, Ireland, and Brittany – and typically date from the Late Neolithic and Early Bronze Age, with most being built from 3000 BC. The best known examples include those at the henge monument at Avebury, the Rollright Stones, and elements within the ring of standing stones at Stonehenge. Scattered examples exist from other parts of Europe. Later, during the Iron Age, stone circles were built in southern Scandinavia. Stone circles are usually grouped in terms of the shape and size of the stones, the span of their radius, and their population within the local area. Although many theories have been advanced to explain their use, usually related to providing a setting for ceremony or ritual, no consensus exists among archaeologists regarding their intended function. Their construction often involved considerable communal effort, including specialist tasks such as planning, quar ...
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University College Cork
University College Cork – National University of Ireland, Cork (UCC) ( ga, Coláiste na hOllscoile Corcaigh) is a constituent university of the National University of Ireland, and located in Cork. The university was founded in 1845 as one of three Queen's Colleges located in Belfast, Cork, and Galway. It became University College, Cork, under the Irish Universities Act of 1908. The Universities Act 1997 renamed the university as National University of Ireland, Cork, and a Ministerial Order of 1998 renamed the university as University College Cork – National University of Ireland, Cork, though it continues to be almost universally known as University College Cork. Amongst other rankings and awards, the university was named Irish University of the Year by ''The Sunday Times'' on five occasions; most recently in 2017. In 2015, UCC was also named as top performing university by the European Commission funded U-Multirank system, based on obtaining the highest number of "A" sco ...
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Megalith
A megalith is a large stone that has been used to construct a prehistoric structure or monument, either alone or together with other stones. There are over 35,000 in Europe alone, located widely from Sweden to the Mediterranean sea. The word was first used in 1849 by the British antiquarian Algernon Herbert in reference to Stonehenge and derives from the Ancient Greek words "mega" for great and " lithos" for stone. Most extant megaliths were erected between the Neolithic period (although earlier Mesolithic examples are known) through the Chalcolithic period and into the Bronze Age. At that time, the beliefs that developed were dynamism and animism, because Indonesia experienced the megalithic age or the great stone age in 2100 to 4000 BC. So that humans ancient tribe worship certain objects that are considered to have supernatural powers. Some relics of the megalithic era are menhirs (stone monuments) and dolmens (stone tables). Types and definitions While "megalith" ...
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Slieve Miskish Mountains
The Slieve Miskish Mountains are a small range of low sandstone mountains found at the extreme south-western tip of the Beara Peninsula of County Cork in Ireland. The name derives from the Irish "Sliabh Mioscais," "the Mountains of Malice." Unlike the Caha Mountains, which lie further north on the peninsula, the Slieve Miskish Mountains lie entirely on the Cork side of the peninsula, part of which belongs to County Kerry. There are only four named mountain peaks in the range: Knocknagallaun, 376 m; Knockgour, 481 m; Knockoura, 490 m; and Miskish Mountain, 386 m. They overshadow the main town on the peninsula, Castletownbere, as well as the village of Allihies on their western slope, which was once the centre of a thriving copper mining industry in the 19th century. The now-abandoned mines and surrounding buildings can still be seen on the mountain slopes above Allihies. See also *List of mountains in Ireland In these lists of mountains in Ireland, those within Northern Ire ...
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Kenmare River
Kenmare () is a small town in the south of County Kerry, Ireland. The name Kenmare is the Anglicisation, anglicised form of ''Ceann Mara'', meaning "head of the sea", referring to the head of Kenmare Bay. Location Kenmare is located at the head of Kenmare Bay (where it reaches the farthest inland), sometimes called the Kenmare River, where the Roughty River (''An Ruachtach'') flows into the sea, and at the junction of the Iveragh Peninsula and the Beara Peninsula. The traditional Irish name of the bay was ''Inbhear Scéine'' from the Insular Celtic languages, Celtic ''Aber and Inver as place-name elements, inver'', which is recorded in the 11th Century narrative ''Lebor Gabála Érenn'' as the arrival point of the Irish mythology, mythological Irish ancestor Partholón. It is also located near the MacGillycuddy's Reeks, Mangerton Mountain and Caha Mountains and is a popular hillwalking destination. Nearby towns and villages are Tuosist, Ardgroom, Glengarriff, Kilgarvan, Killarne ...
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Beara Peninsula
Beara ( ga, Béarra) or the Beara Peninsula is a peninsula on the south-west coast of Ireland, bounded between the Kenmare "river" (actually a bay) to the north side and Bantry Bay to the south. It contains two mountain ranges running down its centre: the Caha Mountains and the Slieve Miskish Mountains. The northern part of the peninsula from Kenmare to near Ardgroom is in County Kerry, while the rest forms the barony of Bear in County Cork. The main features of Beara's landscape were formed during the quaternary period which ended 12,000 years ago. There is evidence of human activity on the peninsula dating from at least 3000 BC. Later it was invaded by Vikings, and in the 17th century became a defensive position for the English Army against French invasion. Its population peaked at 39,000 before the Great Famine; today there are fewer than 6000 living in the area. The peninsula contains a long and varied scenic coast, two mountain ranges and a number of passes, and forms ...
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Provinces Of Ireland
There have been four Provinces of Ireland: Connacht (Connaught), Leinster, Munster, and Ulster. The Irish language, Irish word for this territorial division, , meaning "fifth part", suggests that there were once five, and at times Kingdom_of_Meath, Meath has been considered to be the fifth province; in the medieval period, however, there were often more than five. The number of provinces and their delimitation fluctuated until 1610, when they were permanently set by the English administration of James VI and I, James I. The provinces of Ireland no longer serve administrative or political purposes but function as historical and cultural entities. Etymology In modern Irish language, Irish the word for province is (pl. ). The modern Irish term derives from the Old Irish (pl. ) which literally meant "a fifth". This term appears in 8th-century law texts such as and in the legendary tales of the Ulster Cycle where it refers to the five kingdoms of the "Pentarchy". MacNeill enumer ...
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Drumlins
A drumlin, from the Irish word ''droimnín'' ("littlest ridge"), first recorded in 1833, in the classical sense is an elongated hill in the shape of an inverted spoon or half-buried egg formed by glacial ice acting on underlying unconsolidated till or ground moraine. Assemblages of drumlins are referred to as fields or swarms; they can create a landscape which is often described as having a 'basket of eggs topography'. The low ground between two drumlins is known as a dungeon; dungeons have colder microclimates in winter from settling cold air. Morphology Drumlins occur in various shapes and sizes, including symmetrical (about the long axis), spindle, parabolic forms, and transverse asymmetrical forms. Generally, they are elongated, oval-shaped hills, with a long axis parallel to the orientation of ice flow and with an up-ice (stoss) face that is generally steeper than the down-ice (lee) face. Drumlins are typically 250 to 1,000 meters long and between 120 and 300 meters wide ...
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