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Drumlohan Souterrain And Ogham Stones
Drumlohan souterrain and ogham stones, known locally as the Ogham Cave, is a souterrain with ogham stones forming a National Monument located in County Waterford, Ireland. Location Drumlohan souterrain and ogham stones are located in farmland 4 km (2½ mi) east of Lemybrien. History The ogham stones were carved between 400 and 700 AD. The souterrain is believed to have been constructed around the 9th century AD and is aligned WSW, facing the setting sun. Souterrains were storage sites and places of refuge. In July/August 1867 a local farmer rediscovered the souterrain and ogham stones. In 1936 part of the souterrain was dismantled and some of the ogham stones re-erected above ground. Description Souterrain This souterrain gallery is about 4.9 m (16 ft) long and 1.3 m (4 ft) wide, with a roof height of up to 1.2 m (4 ft). It is constructed of orthostats roofed with lintels, and ten ogham stones were used as lintels and sidestones (some of th ...
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Stradbally, County Waterford
Stradbally (, IPA: anˠˈt̪ˠɾˠaːdʲˌwalʲə is a small village in County Waterford, Ireland. History Medieval period In 1215, King John granted the custody of the counties of Waterford and Desmond (most of Cork and Kerry) to Thomas fitz Anthony. This was a reward for fitz Anthony’s support for the king in fighting rebel barons in England at the time. Thomas fitz Anthony seems to have founded the medieval town of Stradbally, which was situated at the centre of his lordship (he also founded Thomastown in Co. Kilkenny). Thomas fitz Anthony died in 1226 or 1227 and the lordship subsequently passed to one of his sons-in-law, Thomas de Dene. When Thomas de Dene's son Reginald died in 1302, he held a quarter of the town of Stradbally from the king. Stradbally subsequently passed to a branch of the FitzGeralds, Earls of Desmond, who held it until the early 18th century. In 1300, when King Edward I levied his Irish domains to finance his war against Scotland, Stradbally was one ...
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Greenschist
Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures usually produced by regional metamorphism, typically and 2–10 kilobars (). Greenschists commonly have an abundance of green minerals such as chlorite, serpentine, and epidote, and platy minerals such as muscovite and platy serpentine. The platiness gives the rock schistosity (a tendency to split into layers.) Other common minerals include quartz, orthoclase, talc, carbonate minerals and amphibole (actinolite). Greenschist is a general field petrologic term for metamorphic or altered mafic volcanic rock. In Europe, the term ''prasinite'' is sometimes used. A ''greenstone'' is sometimes a greenschist but can also be rock types without any schistosity, especially metabasalt (spilite). However, basalts may remain quite black if primary pyroxene does not revert to chlorite or actinolite. To qualify for the name a rock must also exhibit schistosity or some foliation or layering. The rock i ...
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Ogham Inscriptions
Roughly 400 known ogham inscriptions are on stone monuments scattered around the Irish Sea, the bulk of them dating to the fifth and sixth centuries. Their language is predominantly Primitive Irish, but a few examples record fragments of the Pictish language. Ogham itself is an Early Medieval form of alphabet or cipher, sometimes known as the "Celtic Tree Alphabet". A number of different numbering schemes are used. The most widespread is CIIC, after R. A. S. Macalister (''Corpus Inscriptionum Insularum Celticarum'', Latin for "corpus of Insular Celtic inscriptions"). This covers the inscriptions known by the 1940s. Another numbering scheme is that of the Celtic Inscribed Stones Project, CISP, based on the location of the stones; for example CIIC 1 = CISP INCHA/1. Macalister's (1945) numbers run from 1 to 507, including also Latin and Runic inscriptions, with three additional added in 1949. Ziegler lists 344 Gaelic ogham inscriptions known to Macalister (Ireland and Isle of Ma ...
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National Monuments In County Waterford
National may refer to: Common uses * Nation or country ** Nationality – a ''national'' is a person who is subject to a nation, regardless of whether the person has full rights as a citizen Places in the United States * National, Maryland, census-designated place * National, Nevada, ghost town * National, Utah, ghost town * National, West Virginia, unincorporated community Commerce * National (brand), a brand name of electronic goods from Panasonic * National Benzole (or simply known as National), former petrol station chain in the UK, merged with BP * National Car Rental, an American rental car company * National Energy Systems, a former name of Eco Marine Power * National Entertainment Commission, a former name of the Media Rating Council * National Motor Vehicle Company, Indianapolis, Indiana, USA 1900-1924 * National Supermarkets, a defunct American grocery store chain * National String Instrument Corporation, a guitar company formed to manufacture the first resonator g ...
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On An Ogham Chamber At Drumloghan, In The County Of Waterford (IA Jstor-25497769)
On, on, or ON may refer to: Arts and entertainment Music * On (band), a solo project of Ken Andrews * ''On'' (EP), a 1993 EP by Aphex Twin * ''On'' (Echobelly album), 1995 * ''On'' (Gary Glitter album), 2001 * ''On'' (Imperial Teen album), 2002 * ''On'' (Elisa album), 2006 * ''On'' (Jean album), 2006 * ''On'' (Boom Boom Satellites album), 2006 * ''On'' (Tau album), 2017 * "On" (song), a 2020 song by BTS * "On", a song by Bloc Party from the 2006 album ''A Weekend in the City'' Other media * ''Ön'', a 1966 Swedish film * On (Japanese prosody), the counting of sound units in Japanese poetry * ''On'' (novel), by Adam Roberts * ONdigital, a failed British digital television service, later called ITV Digital * Overmyer Network, a former US television network Places * On (Ancient Egypt), a Hebrew form of the ancient Egyptian name of Heliopolis * On, Wallonia, a district of the municipality of Marche-en-Famenne * Ahn, Luxembourg, known in Luxembourgish as ''On'' * Ontario, a ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ...
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Cup Marks
Cup and ring marks or cup marks are a form of prehistoric art found in the Atlantic seaboard of Europe (Ireland, Wales, Northern England, Scotland, France (Brittany), Portugal, and Spain (Galicia (Spain), Galicia) – and in Mediterranean Europe – Italy (in Alpine valleys and Sardinia), Azerbaijan and Greece (Thessaly and Irakleia (Cyclades)), as well as in Scandinavia (Denmark, Sweden, Norway and Finland) and in Switzerland (at Caschenna in Canton of Grisons, Grisons). Similar forms are also found throughout the world including Australia, Gabon, Greece, Hawaii, India (Bhanpura#Daraki-Chattan Cave survey Bhanpura, Daraki-Chattan), Israel, Mexico, Mozambique and the Americas. The oldest known forms are found from the Fertile Crescent to India. They consist of a wikt:concave, concave depression, no more than a few centimetres across, pecked into a rock surface and often surrounded by concentric circles also etched into the stone. Sometimes a linear channel called a wikt:Special: ...
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County Waterford
County Waterford ( ga, Contae Phort Láirge) is a Counties of Ireland, county in Republic of Ireland, Ireland. It is in the Provinces of Ireland, province of Munster and is part of the South-East Region, Ireland, South-East Region. It is named after the city of Waterford. Waterford City and County Council is the Local government in the Republic of Ireland, local authority for the county. The population of the county at large, including the city, was 116,176 according to the 2016 census. The county is based on the historic Gaelic Ireland, Gaelic territory of the ''Déisi, Déise''. There is an Gaeltacht, Irish-speaking area, Gaeltacht na nDéise, in the south-west of the county. Geography and subdivisions County Waterford has two mountain ranges, the Knockmealdown Mountains and the Comeragh Mountains. The highest point in the county is Knockmealdown, at . It also has many rivers, including Ireland's third-longest river, the River Suir (); and Ireland's fourth-longest river, the ...
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Lintel
A lintel or lintol is a type of beam (a horizontal structural element) that spans openings such as portals, doors, windows and fireplaces. It can be a decorative architectural element, or a combined ornamented structural item. In the case of windows, the bottom span is instead referred to as a sill, but, unlike a lintel, does not serve to bear a load to ensure the integrity of the wall. Modern day lintels are made using prestressed concrete and are also referred to as beams in beam and block slabs or ribs in rib and block slabs. These prestressed concrete lintels and blocks are components that are packed together and propped to form a suspended floor concrete slab. Structural uses In worldwide architecture of different eras and many cultures, a lintel has been an element of post and lintel construction. Many different building materials have been used for lintels. In classical Western architecture and construction methods, by ''Merriam-Webster'' definition, a lintel is a l ...
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