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Carrantuohill
Carrauntoohil or Carrauntoohill ( ; ga, Corrán Tuathail , meaning "Tuathal's sickle") is the highest mountain in Ireland at . It is on the Iveragh Peninsula in County Kerry, close to the centre of Ireland's highest mountain range, MacGillycuddy's Reeks. Carrauntoohil is composed mainly of sandstone, whose glaciation produced distinctive features on the mountain such as the Eagle's Nest corrie and some deep gullies and sharp arêtes in its east and northeastern faces that are popular with rock and winter climbers. As Ireland's highest mountain, Carrauntoohil is popular with mountain walkers, who most commonly ascend via the Devil's Ladder route; however, Carrauntoohil is also climbed as part of longer mountain walking routes in the MacGillycuddy's Reeks range, including the Coomloughra Horseshoe or the MacGillycuddy's Reeks Ridge Walk of the entire mountain range. Carrauntoohil, and most of the range, is held in private ownership and is not part of any Irish national park; h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carrauntoohil Group From Cruach Mhor
Carrauntoohil or Carrauntoohill ( ; ga, Corrán Tuathail , meaning "Tuathal's sickle") is the Lists of mountains in Ireland, highest mountain in Ireland at . It is on the Iveragh Peninsula in County Kerry, close to the centre of Ireland's highest mountain range, MacGillycuddy's Reeks. Carrauntoohil is composed mainly of sandstone, whose glaciation produced distinctive features on the mountain such as the Eagle's Nest cirque, corrie and some deep gullies and sharp arêtes in its east and northeastern faces that are popular with rock and winter climbers. As Ireland's highest mountain, Carrauntoohil is popular with mountain walkers, who most commonly ascend via the Devil's Ladder route; however, Carrauntoohil is also climbed as part of longer mountain walking routes in the MacGillycuddy's Reeks range, including the Coomloughra Horseshoe or the MacGillycuddy's Reeks Ridge Walk of the entire mountain range. Carrauntoohil, and most of the range, is held in private ownership and is n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Furth Mountains In The British Isles
This is a list of Furth mountains in Britain and Ireland by height. Furths are defined as mountains that meet the classification criteria to be a Scottish Munro, including being over in elevation, but which are ''furth'' of (i.e. "outside" of) Scotland. They are also called Welsh Munros, Irish Munros, and English Munros respectively, or the ''three-thousanders,'' as in '' The Welsh 3000 challenge''. Some Furth definitions add a topographical prominence above , akin to a Scottish Murdo, however the official Scottish Mountaineering Club ("SMC") lists includes Furths with a prominence below this level. Applying the Real Munro definition to a Furth, requires a prominence above , akin to a Marilyn, and these 14 Furths are marked with (‡) in the tables below. The SMC lists 34 Furths: six in England, 15 in Wales, and 13 on Ireland. These compare with 282 Munros and 227 Munro Tops in Scotland. 33 have the in prominence to be Murdos. 14 have the of prominence to be Real Munros: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Marilyns In The British Isles
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 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 homophonous with (Marilyn) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordnance Survey Ireland
Ordnance Survey Ireland (OSI; ga, Suirbhéireacht Ordanáis Éireann) is the national mapping agency of Ireland. It was established on 4 March 2002 as a body corporate. It is the successor to the former Ordnance Survey of Ireland. It and the Ordnance Survey of Northern Ireland (OSNI) are the ultimate successors to the Irish operations of the British Ordnance Survey. OSI is part of the Irish public service. OSI has made modern and historic maps of the state free to view on its website. OSI is headquartered at Mountjoy House in the Phoenix Park in Dublin. Mountjoy House was also the headquarters, until 1922, of the Irish section of the British Ordnance Survey. Organisation Under the Ordnance Survey Ireland Act 2001, the Ordnance Survey of Ireland was dissolved and a new corporate body called Ordnance Survey Ireland was established in its place. OSI is now an autonomous corporate body, with a remit to cover its costs of operation from its sales of data and derived products, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beenkeragh
Beenkeragh or Benkeeragh () is the second-highest peak in Ireland, at , on both the Lists of mountains in Ireland#Arderins, Arderin and Lists of mountains in Ireland#Vandeleur-Lynams, Vandeleur-Lynam lists. It is part of the MacGillycuddy's Reeks range in County Kerry. Beenkeragh also gives its name the infamous ''Beenkeragh Ridge'', the narrow rocky arêtes, arete between Beenkeragh and Carrauntoohil, Ireland's highest mountain. Geography Beenkeragh lies to the north of Carrauntoohil ., and is part of the MacGillycuddy's Reeks range in County Kerry. Beenkeragh is joined to Carrauntoohil by a very narrow rocky ridge, or arête, arete, known as the ''Beenkeragh Ridge''. In the middle of the ''Beenkeragh Ridge'' is another other summit called, The Bones () . Beenkeragh is the List of mountains of the British Isles by height, 179th-highest mountain in Britain and Ireland on the Lists of mountains and hills in the British Isles#Simms, Simm classification. Beenkeragh is regar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Bones
The Bones (), at high, is the seventh-highest peak in Ireland on the Lists of mountains in Ireland#Arderins, Arderin list, or the eighth-highest according to the Lists of mountains in Ireland#Vandeleur-Lynams, Vandeleur-Lynam list. It is part of the MacGillycuddy's Reeks in County Kerry, and is a small sharp peak on the dramatic ''Beenkeragh Ridge'', and is sometimes mistaken with ''The Bone'', the north-east spur of Maolán Buí, which descends into the ''Hag's Glen''. Geography The Bones is the highest point on a narrow rocky arête called the ''Beenkeragh Ridge'', situated between Carrauntoohil (Ireland's highest peak), and Beenkeragh (Ireland's second-highest peak), in the MacGillycuddy's Reeks range in County Kerry. The ''Beenkeragh Ridge'' is considered as "intimidating hill-walking conditions", along with the nearby The Big Gun ridge, and is often climbed as part of the ''Carrauntoohil#Coomloughra Horseshoe, Coomloughra Horseshoe''. The Bones is often confused ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beenkeragh Ridge
Beenkeragh or Benkeeragh () is the second-highest peak in Ireland, at , on both the Lists of mountains in Ireland#Arderins, Arderin and Lists of mountains in Ireland#Vandeleur-Lynams, Vandeleur-Lynam lists. It is part of the MacGillycuddy's Reeks range in County Kerry. Beenkeragh also gives its name the infamous ''Beenkeragh Ridge'', the narrow rocky arêtes, arete between Beenkeragh and Carrauntoohil, Ireland's highest mountain. Geography Beenkeragh lies to the north of Carrauntoohil ., and is part of the MacGillycuddy's Reeks range in County Kerry. Beenkeragh is joined to Carrauntoohil by a very narrow rocky ridge, or arête, arete, known as the ''Beenkeragh Ridge''. In the middle of the ''Beenkeragh Ridge'' is another other summit called, The Bones () . Beenkeragh is the List of mountains of the British Isles by height, 179th-highest mountain in Britain and Ireland on the Lists of mountains and hills in the British Isles#Simms, Simm classification. Beenkeragh is regar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
U-shaped Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rocks
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Equatorial Climate
A tropical rainforest climate, humid tropical climate or equatorial climate is a tropical climate sub-type usually found within 10 to 15 degrees latitude of the equator. There are some other areas at higher latitudes, such as the coast of southeast Florida, USA, and Okinawa, Japan that fall into the tropical rainforest climate category. They experience high mean annual temperatures, small temperature ranges, and rain that falls throughout the year. Regions with this climate are typically designated ''Af'' by the Köppen climate classification. A tropical rainforest climate is typically hot, very humid, and wet. Description Tropical rain forests have a type of tropical climate in which there is no dry season—all months have an average precipitation value of at least . There are no distinct wet or dry seasons as rainfall is high throughout the months. One day in a tropical rainforest climate can be very similar to the next, while the change in temperature between day and night m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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