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Craignaw
Craignaw is a hill in the Dungeon Hills, a sub-range of the Galloway Hills range, part of the Southern Uplands of Scotland. Unlike many hills in the Southern Uplands, Craignaw has a complex and rocky summit area, with a long line of crags and rough ground on the east side. The hill is largely composed of granite. Near the north end of the hill is an interesting area of terrain known as the "Deil's Bowlin' Green" where various rounded granite boulders are scatterd at random over an area of nearly horizontal granite slabs. These are believed to be glacial erratics or result from a similar glacier process. On the west side of the hill, near grid reference NX458831, a few hundred meters from the summit is an F-111E Aardvark crash site. The site is marked by a small memorial to the two U.S. Air Force pilots who were killed in the accident (Captains Spaulding and Hetzner). Although the crash happened on 19 December 1979 there are still small amounts of aircraft debris in the area. Wal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Galloway Hills
The Galloway Hills are part of the Southern Uplands of Scotland, and form the northern boundary of western Galloway. They lie within the bounds of the Galloway Forest Park, an area of some of largely uninhabited wild land, managed by Forestry and Land Scotland. The unusual place names reflect a mixture of the Old Norse and Scottish Gaelic languages and hint at the range of influences which have acted on society within the area over the centuries. Location The location of Galloway has been described as follows, "Galloway is contained by sea to the west ( North Channel) and south (Solway Firth), the "Galloway Hills" to the north, and the River Nith to the east". So if we were to say "The hills of Galloway" we would be including all the hills within this area; but as the first sentence implies, the "Galloway Hills" is usually taken to mean a collection of ranges which lie mainly south of Loch Doon and which are not constrained by political boundaries. The boundary between Dumfri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dungeon Hills
The Dungeon Hills are a range of hills in the Galloway Hills range, part of the Southern Uplands of Scotland. The central of three parallel ridges, they are neighboured by the Range of the Awful Hand to the west and the Rhinns of Kells to the east. The range is also perpendicular to the Minnigaff Hills range, immediately south. In total, these four ranges are part of the Galloway Forest Park. The Hills The hills of the range are the lowest and craggiest of the Galloway Hills with the highest, Mullwharchar, reaching 692m. They are split between East Ayrshire and Dumfries and Galloway along the Mullwharchar-Dungeon Hill col, following the Pulskaig Burn. Often regarded as the roughest hills in the Southern Uplands, walks can frequently take longer than anticipated due to the underfoot conditions of tussocks and bog. The range is the most remote of the Galloway Hills as the nearest road link to the north is approximately 2 miles away at Craigmalloch on the banks of Loch Doon, requ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Uplands
The Southern Uplands ( gd, Na Monaidhean a Deas) are the southernmost and least populous of mainland Scotland's three major geographic areas (the other two being the Central Lowlands and the Grampian Mountains and the Highlands, as illustrated in the accompanying map). The term is used both to describe the geographical region and to collectively denote the various ranges of hills and mountains within this region. An overwhelmingly rural and agricultural region, the Southern Uplands are partly forested and contain many areas of open moorland - the hill names in the area are congruent with these characteristics. Geology The Southern Uplands consist mainly of Silurian sedimentary deposits deposited in the Iapetus Ocean 420 million years ago. These rocks were pushed up from the sea bed into an accretionary wedge during the Caledonian orogeny, roughly 400 million years ago ( Ma), when the continents and terranes of Laurentia, Baltica and Avalonia collided. The Caledonian orog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyn (hill)
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Republic of Ireland, Ireland by height. 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 2,011 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) ''Marilyn Monroe, Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donald (hill)
This is a list of Donald mountains in Scotland by height. Lists of mountains and hills in the British Isles#Donalds, Donalds were defined in 1935 by Scottish Mountaineering Club ("SMC") member Percy Donald, as Scottish Lowlands mountains over in height, the general requirement to be called a Lists of mountains and hills in the British Isles#Elevation, "mountain" in the British Isles, and over in prominence, and which also had "sufficient topographical merit" that he outlined in a complex formula. This formula splits Donalds into Donald Hills and Donald Tops. The SMC define Donald Tops as: "elevations in the Scottish Lowlands of at least 2000ft (610m) in height with a drop of at least 50ft (15.2m) between each elevation and any higher elevation. Further, elevations separated from higher elevations by a drop of less than 100ft (30.5m) are required to have "sufficient topographical merit". In addition, the SMC define Donald Hills as being: "defined from Donald Tops, where a Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graham (hill)
This is an overview of the Grahams and a list of them by height. Grahams are defined as Scottish hills between 600 and 762 metres in height, with a minimum prominence, or drop, of 150 metres. The final list of Grahams, with this definition, was published by Alan Dawson in 2022 in the booklet ''Ten Tables of Grahams: The Official List'' and in the book ''Tales from the Grahams: 231 medium-sized hills of Scotland''. Scottish hills between and were referred to as "Elsies" (short for Lesser Corbetts, being "LCs") in April 1992 by British researcher Alan Dawson in his book ''The Relative Hills of Britain''. In November 1992, Fiona Torbet (née Graham) published her own list which did not include the Southern Uplands and had several omissions and inaccuracies. Dawson and Torbet met to discuss the issue and agreed to use Dawson's list but to apply the name ''Grahams'', which they both preferred to ''Elsies''. By definition, all Grahams, given their prominence, are also Marilyns. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of Scotland
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] |
Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Dumfries And Galloway
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Southern Uplands
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donald Mountains
Donald is a masculine given name derived from the Gaelic name ''Dòmhnall''.. This comes from the Proto-Celtic *''Dumno-ualos'' ("world-ruler" or "world-wielder"). The final -''d'' in ''Donald'' is partly derived from a misinterpretation of the Gaelic pronunciation by English speakers, and partly associated with the spelling of similar-sounding Germanic names, such as ''Ronald''. A short form of ''Donald'' is ''Don''. Pet forms of ''Donald'' include ''Donnie'' and ''Donny''. The feminine given name ''Donella'' is derived from ''Donald''. ''Donald'' has cognates in other Celtic languages: Modern Irish ''Dónal'' (anglicised as ''Donal'' and ''Donall'');. Scottish Gaelic ''Dòmhnall'', ''Domhnull'' and ''Dòmhnull''; Welsh '' Dyfnwal'' and Cumbric ''Dumnagual''. Although the feminine given name ''Donna'' is sometimes used as a feminine form of ''Donald'', the names are not etymologically related. Variations Kings and noblemen Domnall or Domhnall is the name of many ancie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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