Stob Coire Sgreamhach
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Stob Coire Sgreamhach
Stob Coire Sgreamhach () is a mountain in Lorn, south of Glen Coe in the Scottish Highlands. Its height is . It is part of the Bidean nam Bian massif and is often considered a subsidiary peak of Bidean, though since the 1997 revision of Munros Tables it has been classified as a separate Munro. To the northeast is the ridge of Beinn Fhada ('the long mountain'). The mountain is usually climbed together with Bidean nam Bian, thus allowing for a traverse of the range. One of the most common routes from Glen Coe is to ascend the head of Coire Gabhail (the 'Hidden Glen' or 'Lost Valley') to reach the bealach between Stob Coire Sgreamhach and Bidean nam Bian. The wide floor of this corrie is hidden from view when seen from Glen Coe, and was used by the local Clan MacDonald to hide livestock, whether their own or stolen on raids. Another route of ascent is via Beinn Fhada, the most easterly of the famous Three Sisters of Glen Coe. This route also starts from Coire Gabhail, but then cli ...
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Coire Gabhail
Coire Gabhail (Corrie of the Bounty, or The Hollow of Capture) is a high level glen in the Bidean nam Bian mountain massif to the south of Glen Coe, Highland, Scotland. Its narrow entrance up the hillside conceals the width of the glen beyond, and it is commonly known as the Hidden Valley or Lost Valley of Glencoe. Access from a bridge crossing the River Coe is by a steep path up beside a narrow wooded ravine. Coire Gabhail runs southwestwards between the steeply-sided ridges of two of "The Three Sisters"; on its left, Beinn Fhada (''Long Hill'') is the eastmost sister, and the central sister Gearr Aonach (''Short Ridge'') on the right of the corrie forms its western side. Further to the west of Gearr Aonach, Coire nan Lochan is enclosed by Aonach Dubh (''Black Ridge''). The southern end of Coire Gabhail is marked by the peak of Stob Coire Sgreamhach on the ridge which then slopes down westwards to its low point at Bealach Dearg, then continues up above cliffs to the summit ...
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List Of Munros
This is a list of Munro mountains and Munro Tops in Scotland by height. Munros are defined as Scottish mountains over in height, and which are on the Scottish Mountaineering Club ("SMC") official list of Munros. In addition, the SMC define Munro Tops, as Scottish peaks above that are not considered Munros. Where the SMC lists a Munro Top, due to "insufficient separation", it will also list the "Parent Peak", a Munro, of the Munro Top. As of 6 September 2012, there were 282 Scottish Munros after the SMC confirmed that Beinn a' Chlaidheimh had been downgraded to a Corbett and as of 10 December 2020, there were 226 Scottish Munro Tops after Stob Coire na Cloiche, a Munro Top to Parent Peak Sgùrr nan Ceathramhnan, was surveyed at 912.5m and was deleted as a Munro Top and downgraded to a Corbett Top. The current SMC list totals 508 summits. While the SMC does not use a prominence metric for classifying Munros, all but one of the 282 Munros have a prominence above , the exception ...
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Mountains And Hills Of Highland (council Area)
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecos ...
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Mountains And Hills Of The Central Highlands
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 ...
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Munros
A Munro () is defined as a mountain in Scotland with a height over , and which is on the Scottish Mountaineering Club (SMC) official list of Munros; there is no explicit topographical prominence requirement. The best known Munro is Ben Nevis (Beinn Nibheis), the highest mountain in the British Isles at . Munros are named after Sir Hugh Munro, 4th Baronet (1856–1919), who produced the first list of such hills, known as ''Munro's Tables'', in 1891. Also included were what Munro considered lesser peaks, now known as Munro Tops, which are also over 3,000 feet but are lower than the nearby primary mountain. The publication of the original list is usually considered to be the epoch event of modern peak bagging. The list has been the subject of subsequent variation and as of 10 December 2020, the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. As of 31 December 2021, 7,098 people had reported ...
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Stob Coire Sgreamhach Summit 11-06-19
Stob may refer to: People * Verity Stob (since 1988), pseudonymous author of IT satirical articles * Ralph Stob (1894–1965), U.S. academic, president (1933–1939) of Calvin College * Henry J. Stob (1908–1996), U.S. academic, namesake of the Calvinist Stob Lectures Places * Stob (village), part of Bulgaria's municipality of Kocherinovo * Stob Earth Pyramids, in Bulgaria's Kyustendil Province * Stob, Scottish prefix for "Mount", as in Stob Binnein, Stob Coire Sgreamhach, Stob Ghabhar, etc. * Stobs Military Camp just outside Hawick Hawick ( ; sco, Haaick; gd, Hamhaig) is a town in the Scottish Borders council area and historic county of Roxburghshire in the east Southern Uplands of Scotland. It is south-west of Jedburgh and south-south-east of Selkirk. It is one of ...
Scotland {{Disambiguation, geo ...
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Glen Etive
Glen Etive ( gd, Gleann Èite) is a glen in the Highlands of Scotland. The River Etive ( gd, Abhainn Èite) rises on the peaks surrounding Rannoch Moor, with several tributary streams coming together at the Kings House Hotel, at the head of Glen Coe. From the Kings House, the Etive flows for about 18 km, reaching the sea loch, Loch Etive. The river and its tributaries are popular with whitewater kayakers and at high water levels it is a test piece of the area and a classic run. At the north end of Glen Etive lie the two mountains known as the "Herdsmen of Etive": Buachaille Etive Mòr and Buachaille Etive Beag. Other peaks accessible from the Glen include Ben Starav, located near the head of Loch Etive, and Beinn Fhionnlaidh on the northern side of the glen. The scenic beauty of the glen has led to its inclusion the Ben Nevis and Glen Coe National Scenic Area, one of 40 such areas in Scotland. A narrow road from the Kings House Hotel runs down the glen, serving several ...
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Glen
A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath".. The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. The designation "glen" also occurs often in place names. Etymology The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. In Manx, ''glan'' is also to be found meaning glen. It is cognate with Welsh ''glyn''. Examples in Northern England, such as Glenridding, Westmorland, or Glendue, near Haltwhistle, Northumberland, are thought to derive from the aforementioned Cumbric cognate, or another Brythonic equivalent. This likely underlies some examples in Southern Scotland. As the name of a river, it is thought to derive from the Irish word ''glan'' meaning clean, or the Welsh word ''gleindid' ...
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Clan MacDonald
Clan Donald, also known as Clan MacDonald ( gd, Clann Dòmhnaill; Mac Dòmhnaill ), is a Highland Scottish clan and one of the largest Scottish clans. The Lord Lyon King of Arms, the Scottish official with responsibility for regulating heraldry in that country, issuing new grants of coats of arms, and serving as the judge of the Court of the Lord Lyon, recognises under Scottish law the ''High Chief of Clan Donald''. Historically the chiefs of the Clan Donald held the title of Lord of the Isles until 1493 and two of those chiefs also held the title of Earl of Ross until 1476. There are also numerous branches to the Clan Donald and several of these have chiefs recognised by the Lord Lyon King of Arms; these are: Clan Macdonald of Sleat, Clan Macdonald of Clanranald, Clan MacDonell of Glengarry, Clan MacDonald of Keppoch, and Clan MacAlister. There are also notable historic branches of Clan Donald without chiefs so-recognised, these are: the Clan MacDonald of Dunnyveg, Clan MacDon ...
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Bealach
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap, saddle, col or notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are often found just above the source of a river, const ...
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Scottish Highlands
The Highlands ( sco, the Hielands; gd, a’ Ghàidhealtachd , 'the place of the Gaels') is a historical region of Scotland. Culturally, the Highlands and the Lowlands diverged from the Late Middle Ages into the modern period, when Lowland Scots replaced Scottish Gaelic throughout most of the Lowlands. The term is also used for the area north and west of the Highland Boundary Fault, although the exact boundaries are not clearly defined, particularly to the east. The Great Glen divides the Grampian Mountains to the southeast from the Northwest Highlands. The Scottish Gaelic name of ' literally means "the place of the Gaels" and traditionally, from a Gaelic-speaking point of view, includes both the Western Isles and the Highlands. The area is very sparsely populated, with many mountain ranges dominating the region, and includes the highest mountain in the British Isles, Ben Nevis. During the 18th and early 19th centuries the population of the Highlands rose to around 300,000, but ...
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Bealach
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap, saddle, col or notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are often found just above the source of a river, const ...
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