|
Benbulbin
Benbulbin (), sometimes Benbulben or Ben Bulben, is a steep-sided and flat-topped mountain in County Sligo, Ireland. It is part of the Dartry Mountains, in an area sometimes called " Yeats Country". Benbulbin, high, formed as a nunatak during the last Ice Age. Benbulbin is a protected site, designated as a County Geological Site by Sligo County Council. Etymology "Benbulbin", "Benbulben" and "Ben Bulben" are all anglicisations of the Irish name "Binn Ghulbain". "Binn" means "peak" or "mountain"; "ghulbain" may mean beak or jaw, or may refer to Conall Gulban, a son of Niall of the Nine Hostages, who was associated with the mountain. Geology Formation Benbulbin was shaped during the ice age, when Ireland was under glaciers. Originally it was a large plateau. Glaciers moving from the northeast to southwest shaped it into its present distinct formation. Rock composition Benbulbin, and the Dartry Mountains as a whole, are composed of limestones on top of mudstones. These ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Benbulben Love
Benbulbin (), sometimes Benbulben or Ben Bulben, is a steep-sided and flat-topped mountain in County Sligo, Ireland. It is part of the Dartry Mountains, in an area sometimes called "William Butler Yeats, Yeats Country". Benbulbin, high, formed as a nunatak during the Last Glacial Period, last Ice Age. Benbulbin is a protected site, designated as a County Geology Site, County Geological Site by Sligo County Council. Etymology "Benbulbin", "Benbulben" and "Ben Bulben" are all anglicisations of the Irish name "Binn Ghulbain". "Binn" means "peak" or "mountain"; "ghulbain" may mean beak or jaw, or may refer to Conall Gulban, a son of Niall of the Nine Hostages, who was associated with the mountain. Geology Formation Benbulbin was shaped during the ice age, when Ireland was under glaciers. Originally it was a large plateau. Glaciers moving from the northeast to southwest shaped it into its present distinct formation. Rock composition Benbulbin, and the Dartry Mountains as a whol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Benbulbin July 2020
Benbulbin (), sometimes Benbulben or Ben Bulben, is a steep-sided and flat-topped mountain in County Sligo, Ireland. It is part of the Dartry Mountains, in an area sometimes called " Yeats Country". Benbulbin, high, formed as a nunatak during the last Ice Age. Benbulbin is a protected site, designated as a County Geological Site by Sligo County Council. Etymology "Benbulbin", "Benbulben" and "Ben Bulben" are all anglicisations of the Irish name "Binn Ghulbain". "Binn" means "peak" or "mountain"; "ghulbain" may mean beak or jaw, or may refer to Conall Gulban, a son of Niall of the Nine Hostages, who was associated with the mountain. Geology Formation Benbulbin was shaped during the ice age, when Ireland was under glaciers. Originally it was a large plateau. Glaciers moving from the northeast to southwest shaped it into its present distinct formation. Rock composition Benbulbin, and the Dartry Mountains as a whole, are composed of limestones on top of mudstones. These roc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dartry Mountains
The Dartry Mountains () are a mountain range in the north west of Ireland, in the north of counties Sligo and Leitrim. They lie between Lough Melvin, Lough Gill and Lough MacNean. The highest point is Truskmore at . Other notable mountains include Benbulbin at , Benwiskin at , and Tievebaun at . The mountains are named after the old '' túath'' of Dartraighe, which was part of the kingdom of Bréifne. The mountains are very close to the Breifne Mountains, which lie to the southeast. The range is a large dissected limestone plateau. Glaciation has carved the distinctive shapes of this mountain range. The range includes the valleys of Glencar, Glenade and Gleniff. Highest peaks Gallery File:Dartrys from Mullaghmore.jpg, Dartry Mountains from Mullaghmore, peaks visible (from left): Truskmore, Benwiskin and Benbulbin File:Front view of Benbulbin (2013).jpg, Benbulbin File:Benwiskin - geograph.org.uk - 1150956.jpg, Benwiskin File:Sruth in Aghaidh an Aird.jpg, Sruth in Ag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Sligo
County Sligo ( , ) is a Counties of Ireland, county in Republic of Ireland, Ireland. It is in the Northern and Western Region and is part of the Provinces of Ireland, province of Connacht. Sligo is the administrative capital and largest town in the county. Sligo County Council is the Local government in the Republic of Ireland, local authority for the county. The population of the county was 70,198 at the 2022 census of Ireland, 2022 census. It is noted for Benbulben Mountain, one of Ireland's most distinctive natural landmarks. History The county was officially formed in 1585 by Sir Henry Sidney, Lord Deputy of Ireland, but did not come into effect until the chaos of the Nine Years' War (Ireland), Nine Years' War ended, in 1603. Its boundaries reflect the Ó Conchobhair Sligigh confederation of Lower Connacht () as it was at the time of the Elizabethan conquest. This confederation consisted of the tuatha, or territories, of Cairbre Drom Cliabh, Cairbre Drumcliabh, Tír Fhíacr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conall Gulban
Conall Gulban (died c. 464) was an Irish king and eponymous ancestor of the ''Cenél Conaill'', who founded the kingdom of '' Tír Chonaill'' in the 5th century, comprising much of what is now County Donegal in Ulster. He was the son of Niall Noígiallach. His by-name Gulban derives from '' Benn Ghulbain'' in the north of modern-day County Sligo, from which centre the sons of Niall set out upon their conquest of the North. King Conall Gulban was murdered by the Masraige at '' Magh Slécht'' in Tullyhaw in what later became Bréifne (Tullyhaw is now a barony in the west of modern-day County Cavan) in 464, on a Friday. He was buried by Saint Caillín at Fenagh in the south of modern-day County Leitrim. He is important in the history of Irish Christianity as he was the first nobleman baptised by Saint Patrick, thus opening the way for the conversion of the ruling classes of Ireland. He appears as a host and companion of Caílte mac Rónáin, one of the central Fianna fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers (Lamination (geology), laminae) less than one centimeter in thickness. This property is called ''Fissility (geology), fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the narrower sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Period
The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth and penultimate period of the Paleozoic era and the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian. The name ''Carboniferous'' means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. Carboniferous is the period during which both terrestrial animal and land plant life was well established. Stegocephalia (four-limbed vertebrates including true tetrapods), whose forerunners (tetrapodomo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dartry Limestone
Dartry () is a small suburb of Dublin, Ireland, often referred to as a corridor between Rathmines area and Milltown. Among the locations in Dartry are Dartry Road, Temple Road, Orwell Park and Palmerston Park. Boundaries Part of Dartry Road is the boundary between the Dáil constituencies of Dublin Bay South and Dublin Rathdown constituencies. This is also the city/county boundary (between the local government areas of the city of Dublin and the county of Dún Laoghaire–Rathdown) and is physically marked by the River Dodder. Transport Darty holds the terminus for the 140 bus (beside Palmerston Park). Dartry was also the terminus for the 12 and 14 Dublin tramways routes. The former terminated outside Palmerston Park and the latter on Dartry Road around Orwell Park. The routes of the old tramways were closed throughout the 1930s to 50s and today the nearest rail link is the Luas stop at Milltown, which is built on the site of the original railway station from the Harcour ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glencar Limestone
The Glencar Limestone is a geologic formation in Ireland. It preserves fossils dating back to the Carboniferous The Carboniferous ( ) is a Geologic time scale, geologic period and System (stratigraphy), system of the Paleozoic era (geology), era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the ... period. See also * List of fossiliferous stratigraphic units in Ireland References * Carboniferous System of Europe Carboniferous Ireland Carboniferous southern paleotropical deposits {{Carboniferous-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyn (hill)
This is a list of Marilyn hills and mountains in the United Kingdom, Republic of Ireland, Ireland and surrounding islands and Stack (geology), sea stacks. Lists of mountains and hills in the British Isles#Marilyns, Marilyns are defined as peaks with a topographic prominence, prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Lists of mountains and hills in the British Isles#Munros, Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,010 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophone, homophonous with (Marilyn) ''Marilyn Monroe, Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. The term ''scree'' is applied both to an unstable steep mountain slope composed of rock fragments and other debris, and to the mixture of rock fragments and debris itself. It is loosely synonymous with talus, material that accumulates at the base of a projecting mass of rock, or talus slope, a landform composed of talus. The term ''scree'' is sometimes used more broadly for any sheet of loose rock fragments mantling a slope, while ''talus'' is used more narrowly for material that accumulates at the base of a cliff or other rocky slope from which it has obviously eroded. Scree is formed by rockfall, which distinguishes it from colluvium. Colluvium is rock fragments or soil deposited by rainwash, sheetwash, or slow downhill creep, usually at the base of gentle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viséan
The Visean, Viséan or Visian is an age in the ICS geologic timescale or a stage in the stratigraphic column. It is the second stage of the Mississippian, the lower subsystem of the Carboniferous. The Visean lasted from to Ma. It follows the Tournaisian age/stage and is followed by the Serpukhovian age/stage. Name and definitions The Viséan Stage was introduced by Belgian geologist André Dumont in 1832. Dumont named this stage after the city of Visé in Belgium's Liège Province. Before being used as an international stage, the Viséan Stage was part of the (West) European regional geologic time scale, in which it followed the Tournaisian Stage and is followed by the Namurian Stage. In the North American regional scale, the Viséan Stage correlates with the upper Osagean, the Meramecian and lower Chesterian stages. In the Chinese regional time scale, it correlates with the lower and middle Tatangian series.; 2006: ''Global time scale and regional stratigraphic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
