|
Reyfad
Reyfad () is a townland in County Fermanagh, Northern Ireland. It lies in the land division of Old Barr, in the civil parish of Boho, County Fermanagh, Boho. The townland has previously been called Rayfadd - 1659, Raffada (Magheryboy) - 1672 and Ráith Fada "long fort" - 1833. This high plateau is known for its extensive cave system (see Caves of the Tullybrack and Belmore hills) and Neolithic stones. The summit of a nearby hill is known as Tullybrack or Reyfad Mountain () but it is in fact situated in the townland of Aghamore, County Fermanagh, also within the Boho area. History Nearby to Tullybrack summit lies Two Dogs (derived from the ga, Sliabh Dá Chon meaning "the hill of the two hounds"), which was the site of an ancient clan battle, as recorded in the Annals of the Four Masters: ''A great number of the men of BreifnySee Breifne. were disabled and slain by Muinter-Feodachain, on the hill of Odhra, in Sliabh-da-Chon. They lost no less than forty men, together wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of The Tullybrack And Belmore Hills
The Caves of the Tullybrack and Belmore hills are a collection of caves in southwest County Fermanagh, Northern Ireland. The region is also described as the West Fermanagh Scarplands by environmental agencies and shares many similar karst features with the nearby Marble Arch Caves Global Geopark. The caves are situated under the hills of Tullybrack () – which incorporates Glenkeel () and Knockmore () – and Belmore (), and feature three major cave systems: Reyfad–Glenkeel, Noon's Hole–Arch Cave and Boho Caves. They have been described as nationally significant by the Northern Ireland Environment Agency. The caves and related features are formed predominantly in the Dartry Limestone Formation – a sequence of rocks assigned to the Asbian sub-stage of the Visean stage of the Carboniferous period. Within this formation, the Knockmore Limestone Member is also an important cave-forming rock sequence. Cave development occurred within the Quaternary period and certain feat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boho, County Fermanagh
Boho (pronounced , ) is a hamlet and a civil parish covering approximately southwest of Enniskillen in County Fermanagh, Northern Ireland. It is situated within Fermanagh and Omagh district. This area contains a high density of historically significant sites stretching from the Neolithic Reyfad Stones, through the Bronze Age/Iron Age (Aghnaglack Tomb) and medieval (High Crosses) to comparatively recent historical buildings such as the Linnett Inn. Boho parish has a high biodiversity of flora and fauna due in part to the niches offered by the limestone karst substrata combined with fen meadow, upland heath and acidic bog. The three mountains found within the parish; namely Glenkeel, Knockmore and Belmore provide a landscape varying from high craggy bluffs, with views of neighbouring counties, to low, flat bogland punctuated by streams and lakes. Below this landscape are two of the three most cave-rich mountains in Northern Ireland, featuring the deepest cave system in Irelan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cup And Ring Mark
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) – 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 Grisons). Similar forms are also found throughout the world including Australia, Gabon, Greece, Hawaii, India ( Daraki-Chattan), Israel, Mexico, Mozambique and the Americas. The oldest known forms are found from the Fertile Crescent to India. They consist of a 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 gutter leads out from the middle. The decoration occurs as a petroglyph on natural boulders and outcrop ... [...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] |
Dowth
Dowth ( ga, Dubhadh) is a Neolithic passage tomb located in the Boyne Valley, County Meath, Ireland. It is one of the three principal tombs of the ''Brú na Bóinne'' World Heritage Sitea landscape of prehistoric monuments including the large passage-tombs of Dowth, Newgrange and Knowth. Unlike Newgrange and Knowth, Dowth has not been independently dated, but its features align it with the other passage tombs which date from between approximately 3200 and 2900 BC. However, Harbison (1970) dates the tomb at 25002000 BC. It is less developed as a tourist attraction than its neighbours, partly because the chamber is much lower, and partly because the decoration is less visible. It was partly excavated, in 1847 by the Royal Irish Academy who dynamited the roof causing the still visible crater, though it was pillaged by Vikings and earlier looters long before that. Archaeological and geophysical field surveys of the entire site, including later monuments, were carried out episodi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Department Of Communications, Energy And Natural Resources
The Department of the Environment, Climate and Communications ( ga, An Roinn Comhshaoil, Aeráide agus Cumarsáide) is a department of the Government of Ireland that is responsible for the telecommunications and broadcasting sectors and regulates, protects and develops the natural resources of Ireland. The head of the department is the Minister for the Environment, Climate and Communications who is assisted by two Ministers of State. Departmental team The official headquarters and ministerial offices of the department are at Adelaide Road, Dublin. The departmental team consists of the following: *Minister for the Environment, Climate and Communications: Eamon Ryan, TD ** Minister of State at the Department of the Environment, Climate and Communications, with special responsibility for Postal Policy and Eircodes: Hildegarde Naughton, TD **Minister of State at the Department of the Environment, Climate and Communications, with special responsibility for Communications and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crinoid
Crinoids are marine animals that make up the class Crinoidea. Crinoids that are attached to the sea bottom by a stalk in their adult form are commonly called sea lilies, while the unstalked forms are called feather stars or comatulids, which are members of the largest crinoid order, Comatulida. Crinoids are echinoderms in the phylum Echinodermata, which also includes the starfish, brittle stars, sea urchins and sea cucumbers. They live in both shallow water and in depths as great as . Adult crinoids are characterised by having the mouth located on the upper surface. This is surrounded by feeding arms, and is linked to a U-shaped gut, with the anus being located on the oral disc near the mouth. Although the basic echinoderm pattern of fivefold symmetry can be recognised, in most crinoids the five arms are subdivided into ten or more. These have feathery pinnules and are spread wide to gather planktonic particles from the water. At some stage in their lives, most crinoids have ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brachiopods
Brachiopods (), phylum Brachiopoda, are a phylum of trochozoan animals that have hard "valves" (shells) on the upper and lower surfaces, unlike the left and right arrangement in bivalve molluscs. Brachiopod valves are hinged at the rear end, while the front can be opened for feeding or closed for protection. Two major categories are traditionally recognized, articulate and inarticulate brachiopods. The word "articulate" is used to describe the tooth-and-groove structures of the valve-hinge which is present in the articulate group, and absent from the inarticulate group. This is the leading diagnostic skeletal feature, by which the two main groups can be readily distinguished as fossils. Articulate brachiopods have toothed hinges and simple, vertically-oriented opening and closing muscles. Conversely, inarticulate brachiopods have weak, untoothed hinges and a more complex system of vertical and oblique (diagonal) muscles used to keep the two valves aligned. In many brachiopods, a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Ireland Environment Agency
The Northern Ireland Environment Agency (NIEA) is an executive agency within the Department of Agriculture, Environment and Rural Affairs (DAERA). It is responsible for conservation of Northern Ireland's environment and natural heritage. Originally part of the Department of the Environment (DOENI), the agency was called the Environment and Heritage Service (EHS) until 1 July 2008, and also had responsibility for the historic environment. On 16 May 2016 the DOENI was dissolved and NIEA became part of DAERA. At the same time, the historic environment functions of NIEA were transferred to the Department for Communities. NIEA is responsible for a range of protected areas in Northern Ireland, including eight areas of outstanding natural beauty, 47 national nature reserves, 43 special areas of conservation, and 10 special protection areas. The NIEA employs 630 people as of 2020. Equivalent bodies in other parts of the United Kingdom * England: Environment Agency, Natural England ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Breccia
Breccia () is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix. The word has its origins in the Italian language, in which it means "rubble". A breccia may have a variety of different origins, as indicated by the named types including sedimentary breccia, tectonic breccia, igneous breccia, impact breccia, and hydrothermal breccia. A megabreccia is a breccia composed of very large rock fragments, sometimes kilometers across, which can be formed by landslides, impact events, or caldera collapse. Types Breccia is composed of coarse rock fragments held together by cement or a fine-grained matrix. Like conglomerate, breccia contains at least 30 percent of gravel-sized particles (particles over 2mm in size), but it is distinguished from conglomerate because the rock fragments have sharp edges that have not been worn down. These indicate that the gravel was deposited very close to its source area, since otherwise th ... [...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] |
_01_svg.svg "Click for more on -> Brachiopods")
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")