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Stob Ghabhar
Stob Ghabhar is a mountain in the Scottish Highlands, part of the Black Mount group. It is a Munro with a height of . Stob Ghabhar lies northwest of Bridge of Orchy and stands on the border of the Argyll and Highland council areas. Overview Stob Ghabhar is well seen from the east and is a familiar sight to motorists on the A82 road as it skirts the western edge of Rannoch Moor. The mountains eastern corries formed by the headwaters of the River Ba look impressive from this direction as does the neighbouring mountain of Stob a' Choire Odhair with which Stob Ghabhar is usually climbed. It reaches a height of and qualifies as a Munro and a Marilyn. The mountain's name translates from Scottish Gaelic as "goats' peak".All above reference books give this translation. Goats were often encouraged by shepherds on mountains with precipitous cliffs such as Stob Ghabhar to keep sheep away from the steep drops. Geography Stob Ghabhar is regarded as the finest of the four Munro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Tulla
Loch Tulla ( gd, Loch Toilbhe ) is a small loch at near Bridge of Orchy and Glen Coe in Scotland and in the central highlands. It contains salmon some of which are bred locally. The loch is 2.5 miles in length and an average 0.5 miles in width, with a mean depth of 33 feet and a maximum depth of 84 feet. The river River Orchy flows from the southeastern side of the loch. It lies north-east of the Inveroran Hotel, a popular West Highland Way stop off point close to Bridge of Orchy. History In the 1892 annual report of the Fishery Board for Scotland, Loch Tulla was noted as having trout fishing that was unsurpassed in Scotland sixty years prior, but had since been ruined by the introduction of pike by Lord Breadalbane after being advised by "some dangerous person" to do so in 1848. The Marquis of Breadalbane was obliged to use nets to keep the pike numbers low in the loch for fishing purposes. References Tulla Tulla () is a market town in County Clare, Ireland. It is s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Creise
Creise ( gd, A' Chrèise) is a mountain summit in the Black Mount range, in the Scottish Highlands. It overlooks the northern end of Glen Etive and its height is . Creise is one of four Munros in the Black Mount, along with Meall a' Bhuiridh, Stob Ghabhar and Stob a' Choire Odhair. The mountain is a long and flattish ridge, whose highest point was unnamed until 1981. It is popular with cross-country skiers, being near the White Corries ski area from where it is often climbed along with adjoining Meall a' Bhuiridh. The steep and craggy northern buttress, Sròn na Crèise, is well seen from the A82 road road and the Kings House Hotel. Name The mountain is a long and flattish ridge. Until 1981, it seems the only named parts of the ridge were ''Sròn na Crèise'' and ''Stob a' Ghlais Choire'' at the northern end, and ''Clach Leathad'' (Clachlet) at the southern end. The highest point was apparently unnamed until then, being only one meter higher than ''Clach Leathad''. It see ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Tay
The Firth of Tay (; gd, Linne Tatha) is a firth on the east coast of Scotland, into which the River Tay (Scotland's largest river in terms of flow) empties. The firth is surrounded by four council areas: Fife, Perth and Kinross, City of Dundee, and Angus. Its maximum width (at Invergowrie) is . Two bridges span the firth: the Tay Road Bridge and the Tay Rail Bridge. The marshy Mugdrum Island is the only major island in the firth. The Firth of Tay in Antarctica was discovered in 1892–93 by Captain Thomas Robertson of the Dundee whaling expedition and named by him after the one in Scotland. He also named nearby Dundee Island in honour of the main city on the firth. Natural heritage The Firth of Tay and the Eden Estuary (which lies to the south of the firth) were designated as Special Protection Areas on 2 February 2000, as Ramsar wetlands a few months later (on 28 July 2000), and as Special Areas of Conservation five years later (on 17 March 2005). Several parts of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tay
The River Tay ( gd, Tatha, ; probably from the conjectured Brythonic ''Tausa'', possibly meaning 'silent one' or 'strong one' or, simply, 'flowing') is the longest river in Scotland and the seventh-longest in Great Britain. The Tay originates in western Scotland on the slopes of Ben Lui ( gd, Beinn Laoigh), then flows easterly across the Highlands, through Loch Dochart, Loch Iubhair and Loch Tay, then continues east through Strathtay (see Strath), in the centre of Scotland, then southeasterly through Perth, where it becomes tidal, to its mouth at the Firth of Tay, south of Dundee. It is the largest river in the British Isles by measured discharge. Its catchment is approximately , the Tweed's is and the Spey's is . The river has given its name to Perth's Tay Street, which runs along its western banks for . Course The Tay drains much of the lower region of the Highlands. It originates on the slopes of Ben Lui (''Beinn Laoigh''), around from the west coast town of Oban, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Rannoch
Loch Rannoch (Scottish Gaelic: ''Loch Raineach'') is a freshwater loch in Perth and Kinross, Scotland. It is over long in a west–east direction with an average width of about , and is deepest at its eastern end, reaching a depth of .Tom Weir. ''The Scottish Lochs''. pp. 69-75. Published by Constable and Company, 1980. The River Tummel begins at its eastern end, where the small village of Kinloch Rannoch can be found, whilst the wild expanse of Rannoch Moor extends to the west of the loch. The area surrounding Loch Rannoch, along with Rannoch Moor itself, was formerly part of the native Caledonian Forest that stretched across much of Northern Scotland. Native forest is now largely absent from much of the area, due partly to logging, and partly to the climate becoming wetter, and Loch Rannoch is now largely surrounded by commercial forestry and open hillsides,Ordnance Survey. ''Landranger'' 1:50000 Sheet 42. Glen Garry and Loch Rannoch. although a small area remains at the Blac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Awe
Loch Awe (Scottish Gaelic: ''Loch Obha'') is a large body of freshwater in Argyll and Bute, Scottish Highlands. It has also given its name to a village on its banks, variously known as Loch Awe or Lochawe. There are islands within the loch such as Innis Chonnell and Inishail. The loch It is the third largest freshwater loch in Scotland with a surface area of . It is the longest freshwater loch in Scotland, measuring from end to end with an average width of . The loch runs approximately south-west to north-east, roughly parallel to the two sea lochs of Loch Etive and Loch Fyne. Via the River Awe and Loch Etive it drains westward from its northern end and thus into the Atlantic Ocean. At the narrowest section of the loch are North Port (Taychreggan Hotel) and South Port (Portsonachan Hotel). Once used by cattle drovers, a ferry ran between these shores to facilitate crossing to markets beyond. The Transatlantic Cable, which runs through the village of Kilchrenan, was laid acro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Orchy
Glen Orchy ( gd, Gleann Urchaidh) is a glen in Argyll and Bute, Scotland. It runs from Bridge of Orchy to Dalmally. Geography Glen Orchy is about 17 km or 11 miles long, and runs south-west from Bridge of Orchy () to Dalmally () following the River Orchy through the Caledonian Forest. There are no settlements in the glen: just a few isolated buildings. The Eas Urchaidh and Eas a’ Chathaidh are waterfalls within the glen. The continuation westward past Dalmally to Loch Awe is known as the Strath of Orchy. The B8074 road runs the length of Glen Orchy. Name Glen Orchy was known by the by-name of Gleann Urchaidh nam badan (Glen Orchy of the copses), and the parish of Glen Orchy was An Dìseart (the hermitage), a name appearing in Clachan an Dìseirt (the village of the hermitage), the local Gaelic name of the village of Dalmally. History Glen Orchy was one of the major homes of Clan Gregor until the clan was outlawed in 1603 by King James VI. The settlement of Gleno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oban
Oban ( ; ' in Scottish Gaelic meaning ''The Little Bay'') is a resort town within the Argyll and Bute council area of Scotland. Despite its small size, it is the largest town between Helensburgh and Fort William. During the tourist season, the town can have a temporary population of up to over 24,000 people. Oban occupies a setting in the Firth of Lorn. The bay forms a near perfect horseshoe, protected by the island of Kerrera; and beyond Kerrera, the Isle of Mull. To the north, is the long low island of Lismore and the mountains of Morvern and Ardgour. Pre-history and archaeology Humans have used the site where Oban now stands since at least Mesolithic times, as evidenced by archaeological remains of cave dwellers found in the town. Just outside the town, stands Dunollie Castle, on a site that overlooks the main entrance to the bay and has been fortified since the Bronze Age. Just to the north of Oban, at Dunstaffnage, excavations in 2010, by Argyll Archaeology, in advanc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Etive
Loch Etive (Scottish Gaelic, ''Loch Eite'') is a 30 km sea loch in Argyll and Bute, Scotland. It reaches the sea at Connel, 5 km north of Oban. It measures 31.6 km (19 miles) long and from 1.2 km ( mile) to wide. Its depth varies greatly, up to a maximum of . The name ''Etive'' is believed to mean "little fierce one" from the Gaelic goddess associated with the loch. It heads east for half its length alongside the main road and rail link to Oban, before heading northeast into mountainous terrain. A road along Glen Etive makes the head of the loch accessible from Glen Coe. The narrow mouth of the loch results in its most unusual feature, the Falls of Lora. Part of the north bank has been designated a Special Area of Conservation in particular due to old sessile oak woods. A small colony of around 20 common seals is resident in Loch Etive. Just seaward of the mouth of the loch is Dunstaffnage Castle. This was a stronghold of the kingdom of Dál Riata ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Couloir
A ''couloir'' (, "passage" or "corridor") is a narrow gully with a steep gradient in a mountainous terrain.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, p. 121. . Geology A couloir may be a seam, scar, or fissure, or vertical crevasse in an otherwise solid mountain mass. Though often hemmed in by sheer cliff walls, couloirs may also be less well-defined, and often simply a line of broken talus or scree ascending the mountainside and bordered by trees or other natural features. Couloirs are especially significant in winter months when they may be filled in with snow or ice, and become much more noticeable than in warmer months when most of the snow and ice may recede. These physical features make the use of couloirs popular for both mountaineering and extreme skiing Extreme skiing is performed on long, steep (typically from 45 to 60+ degrees, or grades of 100 to 170 percent) slopes in mountainous terrain. The French coined the term 'Le Ski Ext ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch
''Loch'' () is the Scottish Gaelic, Scots language, Scots and Irish language, Irish word for a lake or sea inlet. It is Cognate, cognate with the Manx language, Manx lough, Cornish language, Cornish logh, and one of the Welsh language, Welsh words for lake, llwch. In English English and Hiberno-English, the Anglicisation, anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuary, estuaries, straits or bays. Background This name for a body of water is Insular Celtic languages, Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish language, Irish, Manx language, Manx, and has been borrowed into Scots language, Lowland Scots, Scottish English, Iri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
