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Inch, County Kerry
Inch () is a small coastal settlement and townland on the Dingle Peninsula in County Kerry, Ireland. Inch Strand, in Inch townland, is on a long sand spit and dune system which reaches into Dingle Bay. The R561 regional road passes through the area. Evidence of ancient settlement in the area includes a number of midden, ringfort and ecclesiastical enclosure sites in Inch and Inch East townlands. The graveyard enclosure, in Inch East, contains a ruined single-cell church which dates to at least the 13th century. Inch Strand, also known as Inch Beach, is a spit which is 5 km in length and, together with its dune system, forms part of the Special Area of Conservation A Special Area of Conservation (SAC) is defined in the European Union's Habitats Directive (92/43/EEC), also known as the ''Directive on the Conservation of Natural Habitats and of Wild Fauna and Flora''. They are to protect the 220 habitats and ap ... at Castlemaine Harbour. References Towns and villag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inch Village - Geograph
Measuring tape with inches The inch (symbol: in or ″) is a unit of length in the British imperial and the United States customary systems of measurement. It is equal to yard or of a foot. Derived from the Roman uncia ("twelfth"), the word ''inch'' is also sometimes used to translate similar units in other measurement systems, usually understood as deriving from the width of the human thumb. Standards for the exact length of an inch have varied in the past, but since the adoption of the international yard during the 1950s and 1960s the inch has been based on the metric system and defined as exactly 25.4 mm. Name The English word "inch" ( ang, ynce) was an early borrowing from Latin ' ("one-twelfth; Roman inch; Roman ounce"). The vowel change from Latin to Old English (which became Modern English ) is known as umlaut. The consonant change from the Latin (spelled ''c'') to English is palatalisation. Both were features of Old English phonology; see a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Townland
A townland ( ga, baile fearainn; Ulster-Scots: ''toonlann'') is a small geographical division of land, historically and currently used in Ireland and in the Western Isles in Scotland, typically covering . The townland system is of Gaelic origin, pre-dating the Norman invasion, and most have names of Irish origin. However, some townland names and boundaries come from Norman manors, plantation divisions, or later creations of the Ordnance Survey.Connolly, S. J., ''The Oxford Companion to Irish History, page 577. Oxford University Press, 2002. ''Maxwell, Ian, ''How to Trace Your Irish Ancestors'', page 16. howtobooks, 2009. The total number of inhabited townlands in Ireland was 60,679 in 1911. The total number recognised by the Irish Place Names database as of 2014 was 61,098, including uninhabited townlands, mainly small islands. Background In Ireland a townland is generally the smallest administrative division of land, though a few large townlands are further divided into h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dingle Peninsula
The Dingle Peninsula ( ga, Corca Dhuibhne; anglicised as Corkaguiny, the name of the corresponding barony) is the northernmost of the major peninsulas in County Kerry. It ends beyond the town of Dingle at Dunmore Head, the westernmost point of Ireland and arguably Europe. Name The Dingle Peninsula is named after the town of Dingle. The peninsula is also commonly called ''Corca Dhuibhne'' (Corcu Duibne) even when those referring to it are speaking in English. ''Corca Dhuibhne'', which means "seed or tribe of Duibhne" (a Goddess, a Gaelic clan name), takes its name from the ''túath'' (people, nation) of ''Corco Dhuibhne'' who occupied the peninsula in the Middle Ages and who also held a number of territories in the south and east of County Kerry. Geography The peninsula exists because of the band of sandstone rock that forms the Slieve Mish mountain range at the neck of the peninsula, in the east, and the Brandon Group of mountains, and the Mountains of the Central Dingle Peni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Kerry
County Kerry ( gle, Contae Chiarraí) is a county in Ireland. It is located in the South-West Region and forms part of the province of Munster. It is named after the Ciarraige who lived in part of the present county. The population of the county was 155,258 at the 2022 census, A popular tourist destination, Kerry's geography is defined by the MacGillycuddy's Reeks mountains, the Dingle, Iveragh and Beara peninsulas, and the Blasket and Skellig islands. It is bordered by County Limerick to the north-east and Cork County to the south and south-east. Geography and subdivisions Kerry is the fifth-largest of Ireland's 32 traditional counties by area and the 16th-largest by population. It is the second-largest of Munster's six counties by area, and the fourth-largest by population. Uniquely, it is bordered by only two other counties: County Limerick to the east and County Cork to the south-east. The county town is Tralee although the Catholic diocesan seat is Killarney, whi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand Spit
A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sediment in the direction the waves are breaking, forming an above-water spit. Without the compl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dune System
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dingle Bay
Dingle Bay (''Bá an Daingin'' in Irish) is a bay located in County Kerry, western Ireland. The outer parts of the Dingle Peninsula and Dingle Bay mark one of the westernmost points of mainland Ireland. The harbour town of Dingle lies on the north side of the bay. Geography The bay runs approximately from northeast to southwest into the Atlantic Ocean. It is approximately wide at the head, and wide at the entrance. It is flanked on the north by the Dingle Peninsula, and on the south by the Iveragh Peninsula. The River Maine enters the bay at its head. The harbour town of Dingle lies on the north side of the bay. Other settlements overlooking the bay include Ventry, Ballymeentrant, Beenbane, and Kinard, and Annascaul and Glenbeigh lie near the bay. Killorglin lies at the head of the bay at the mouth of the River Laune. There are no notable islands within the bay, but towards the head, several peninsulas, in particular Inch Strand, extend a significant distance across i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
R561 Road (Ireland)
The R561 road is a regional road in Ireland. It is on the Dingle Peninsula in County Kerry. Part of the road is on the Wild Atlantic Way. Inch Beach, beginning at the R561, is a wide, sandy beach long. The beach dunes have yielded archaeological remains of ancient dwelling sites. The R561 travels west from the N22 at Farranfore. The road joins the N70 from Brackhill to Castlemaine. The R561 continues west from Castlemaine along the north shore of Castlemaine Harbour to Inch and Inch Beach. The road then travels along the north shore of Dingle Bay before joining the N86 near Annascaul Annascaul or Anascaul () is a village on the Dingle Peninsula in County Kerry, Ireland. It is situated 32.9 kilometres west of Tralee on the N86 Tralee - Dingle national secondary road near its junction with the R561 regional road to Castlema .... The R561 is long. References Regional roads in the Republic of Ireland Roads in County Kerry {{Ireland-road-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midden
A midden (also kitchen midden or shell heap) is an old dump for domestic waste which may consist of animal bone, human excrement, botanical material, mollusc shells, potsherds, lithics (especially debitage), and other artifacts and ecofacts associated with past human occupation. These features provide a useful resource for archaeologists who wish to study the diets and habits of past societies. Middens with damp, anaerobic conditions can even preserve organic remains in deposits as the debris of daily life are tossed on the pile. Each individual toss will contribute a different mix of materials depending upon the activity associated with that particular toss. During the course of deposition sedimentary material is deposited as well. Different mechanisms, from wind and water to animal digs, create a matrix which can also be analysed to provide seasonal and climatic information. In some middens individual dumps of material can be discerned and analysed. Shells A shell mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ringfort
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spit (landform)
A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sediment in the direction the waves are breaking, forming an above-water spit. Without the co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Special Area Of Conservation
A Special Area of Conservation (SAC) is defined in the European Union's Habitats Directive (92/43/EEC), also known as the ''Directive on the Conservation of Natural Habitats and of Wild Fauna and Flora''. They are to protect the 220 habitats and approximately 1,000 species listed in annex I and II of the directive which are considered to be of European interest following criteria given in the directive. They must be chosen from the Sites of Community Importance by the member states and designated SAC by an act assuring the conservation measures of the natural habitat. SACs complement Special Protection Areas and together form a network of protected sites across the European Union called Natura 2000. This, in turn, is part of the Emerald network of Areas of Special Conservation Interest (ASCIs) under the Berne Convention. Assessment methodology in the United Kingdom Prior to being designated as a Special Area of Conservation (SAC), sites have been assessed under a two-stage process ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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