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Inchnadamph
Inchnadamph is a hamlet in Assynt, Sutherland, Scotland. The name is an anglicisation of the Gaelic name Innis nan Damh meaning 'meadow of the stags'. Assynt is a remote area with a low population density. Inchnadamph contains a few houses, a lodge, a hotel and a historic old church, graveyard and mausoleum. History Bone Caves The 'Bone Caves' of Inchnadamph contain relics of Eurasian lynx, brown bear, Arctic fox, reindeer (dated to 47,000 BCE), the only evidence of polar bears so far found in Scotland, and human skeletons dated to the 3rd millennium BCE. Murray, W.H. (1977) ''The Companion Guide to the West Highlands of Scotland.'' London. Collins. Murray states the skeletons were dated to 6000 BC. The skeleton of a bear thought to be 11,000 years old or more was removed from the caves in 2008. The bones were found by cavers in 1995, deep in the ''Uamh an Claonaite'' system and have been examined by the National Museums Scotland to determine the age and species. It is presum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inchnadamph
Inchnadamph is a hamlet in Assynt, Sutherland, Scotland. The name is an anglicisation of the Gaelic name Innis nan Damh meaning 'meadow of the stags'. Assynt is a remote area with a low population density. Inchnadamph contains a few houses, a lodge, a hotel and a historic old church, graveyard and mausoleum. History Bone Caves The 'Bone Caves' of Inchnadamph contain relics of Eurasian lynx, brown bear, Arctic fox, reindeer (dated to 47,000 BCE), the only evidence of polar bears so far found in Scotland, and human skeletons dated to the 3rd millennium BCE. Murray, W.H. (1977) ''The Companion Guide to the West Highlands of Scotland.'' London. Collins. Murray states the skeletons were dated to 6000 BC. The skeleton of a bear thought to be 11,000 years old or more was removed from the caves in 2008. The bones were found by cavers in 1995, deep in the ''Uamh an Claonaite'' system and have been examined by the National Museums Scotland to determine the age and species. It is presum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Assynt
Loch Assynt ( gd, Loch Asaint) is a freshwater loch in Sutherland, Scotland, east-north east of Lochinver. Situated in a spectacular setting between the heights of Canisp, Quinag and Beinn Uidhe, it receives the outflow from Lochs Awe, Maol a' Choire, and Leitir Easaich. It discharges into the sea at Loch Inver, via the river Inver. The general trend of the loch is west-northwest and east-southeast, while the western end bends sharply at Loch Assynt lodge to the southwest.Murray and Pullar (1910"Lochs of the Inver Basin"Page 149, Volume II, Part I. National Library of Scotland. Retrieved 16 July 2021 The loch is long, and about in maximum breadth. The total area is approximately and its drainage basin is over . The total volume of the loch is approximately and the maximum depth is . There is excellent fishing for trout, sea-trout, and salmon. Ardvreck Castle, once held by the MacLeods and Mackenzies, occupies a promontory on the north shore, west of Inchnadamph. The e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assynt Church Inchnadamph Scotland Jul14 DSC 5263
Assynt ( gd, Asainn or ) is a sparsely populated area in the south-west of Sutherland, lying north of Ullapool on the west coast of Scotland. Assynt is known for its landscape and its remarkable mountains, which have led to the area, along with neighbouring Coigach, being designated as the Assynt-Coigach National Scenic Area, one of 40 such areas in Scotland. The western part of Assynt has many distinctively shaped mountains, including Quinag, Canisp, Suilven and Ben More Assynt, that rise steeply from the surrounding "cnoc and lochan" scenery. These can often appear higher than their actual height would indicate due to their steep sides and the contrast with the moorland from which they rise. Many of the most distinctive peaks such as Suilven were formed during the last Ice Age, when they were left exposed above the ice sheet as nunataks, and they now remain as inselbergs of highly eroded Torridonian sandstone sitting on a bedrock of much older Lewisian gneiss. The Moine Thrus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assynt
Assynt ( gd, Asainn or ) is a sparsely populated area in the south-west of Sutherland, lying north of Ullapool on the west coast of Scotland. Assynt is known for its landscape and its remarkable mountains, which have led to the area, along with neighbouring Coigach, being designated as the Assynt-Coigach National scenic area (Scotland), National Scenic Area, one of 40 such areas in Scotland. The western part of Assynt has many distinctively shaped mountains, including Quinag, Canisp, Suilven and Ben More Assynt, that rise steeply from the surrounding "cnoc and lochan" scenery. These can often appear higher than their actual height would indicate due to their steep sides and the contrast with the moorland from which they rise. Many of the most distinctive peaks such as Suilven were formed during the last Ice age, Ice Age, when they were left exposed above the ice sheet as nunataks, and they now remain as inselbergs of highly eroded Torridonian sandstone sitting on a bedrock of mu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ben Peach
Benjamin Neeve Peach (6 September 1842 – 29 January 1926) was a British geologist. Life Peach was born at Gorran Haven in Cornwall on 6 September 1842 to Jemima Mabson and Charles William Peach, an amateur British naturalist and geologist. He was educated at the Royal School of Mines in London and then joined the Geological Survey in 1862 as a geologist, moving to the Scottish branch in 1867. He is best remembered for his work on the Northwest Highlands and Southern Uplands with his friend and colleague John Horne, where they resolved the long-running "Highlands Controversy" with their 1907 publication of ''The Geological Structure of the North-West Highlands of Scotland''. In 1881 he was elected a Fellow of the Royal Society of Edinburgh. His proposers were Archibald Geikie, Sir Charles Wyville Thomson, Peter Guthrie Tait and Robert Gray. He won the Society's Neill Prize for the period 1883–86. He served as the Society's Vice President from 1912 to 1917. He was electe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Horne
John Horne PRSE FRS FRSE FEGS LLD (1 January 1848 – 30 May 1928) was a Scottish geologist. He served as President of the Royal Society of Edinburgh from 1915 to 1919. Life Horne was born on 1 January 1848, in Campsie, Stirlingshire, the son of Janet (''née'' Braid) and James Horne of Newmill, a farmer. He was educated at the High School, Glasgow, and the University of Glasgow where he studied under Lord Kelvin. He left university without graduating at the age on 19. In 1867 he joined the Scottish Branch of HM Geological Survey as an assistant and became an apprentice to Ben Peach. The two soon became good friends and collaborators. Horne was involved in mapping the Central Lowlands. Horne was a logical thinker and writer, complementing Peach's skills of resolving the internal structure of mountains by looking at the surface rocks. Thia approach allowed them to resolve a long-running debate on the "Highlands Controversy" in the 1907 publication of ''The Geological Struct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Geological Structure Of The North-West Highlands Of Scotland
The Highlands controversy was a scientific controversy which started between British geologists in the middle of the nineteenth century concerning the nature of the rock strata in the Northwest Highlands of Scotland. The debate became contentious, even acrimonious, because of some of the personalities involved and because it pitted professional geologists of the Geological Survey against academic and amateur geologists. An initial resolution was achieved by about 1886 but the great complexity and scientific importance of the discovery of the Moine Thrust Belt and the geological processes involved in its creation led to field work continuing for a further twenty years culminating in the 1907 publication by the Geological Survey of a book of fundamental geological significance: ''The Geological Structure of the North-West Highlands of Scotland''. The acrimony was an important factor in the political decision to set up the Wharton Committee of 1899 to review the state-funded Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ardvreck Castle
Ardvreck Castle is a castle, now ruinous, standing on a rocky promontory in Loch Assynt, Sutherland, Scotland, UK. The structure dates from about 1490 and is associated with the then landowners, the Macleods of Assynt. History of Ardvreck The castle was built in the 15th century by the MacLeods of Assynt. It replaced Assynt Castle which was four miles north-west of Inchnadamph. Ardvreck is notable as the place where the royalist James Graham, 1st Marquess of Montrose was handed over in 1650 to the Covenanter forces by MacLeod, Laird of Assynt after the Battle of Carbisdale. The true history of this event is unclear. One account is that MacLeod, loyal to the Covenanters, arrested the weary, fleeing, Montrose and held him. Another is that he provided comfortable shelter, but betrayed Montrose for a £25,000 reward. Clan Mackenzie attacked and captured Ardvreck Castle in 1672, and then took control of the Assynt lands. In 1726 they constructed a more modern manor house nearb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knockan Crag
Knockan Crag ( gd, Creag a' Chnocain, "crag of the small hill")The Story of Knockan Crag National Nature Reserve. p. ii. lies within the North West Highlands Geopark in the Assynt region of Scotland north of Ullapool. During the nineteenth century Knockan Crag became the subject of much debate when geologists noted that the Moine schists at the top of the crag appeared to be older than the Cambrian and Ordovician rocks such as Durness limestone lower down. Disagreements over the processes that could have caused this to occur were referred to at the time as the " Highlands Controversy". The argument was primarily between Roderick Murchison and Archibald Geikie on the one hand and James Nicol and Charles Lapworth on the other. Murchison and Geikie believed the sequence was wrong and that the Moine schists must be the younger rocks. The controversy was finally resolved by the work of Ben Peach and John Horne whose 1907 paper on the subject remains a classic text. Peach and Horne de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moine Thrust Belt
The Moine Thrust Belt or Moine Thrust Zone is a linear tectonic feature in the Scottish Highlands which runs from Loch Eriboll on the north coast south-west to the Sleat peninsula on the Isle of Skye. The thrust belt consists of a series of thrust faults that branch off the Moine Thrust itself. Topographically, the belt marks a change from rugged, terraced mountains with steep sides sculptured from weathered igneous, sedimentary and metamorphic rocks in the west to an extensive landscape of rolling hills over a metamorphic rock base to the east. Mountains within the belt display complexly folded and faulted layers and the width of the main part of the zone varies up to , although it is significantly wider on Skye. Discovery The presence of metamorphic gneisses and schists lying apparently stratigraphically above sedimentary rocks of lower Paleozoic age in the Northwest Highlands had been known since the early 19th century, convincing Roderick Murchison that the change was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Scotland
The geology of Scotland is unusually varied for a country of its size, with a large number of differing geological features.Keay & Keay (1994) page 415. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlands is a rift valley mainly comprising Palaeozoic formations; and the Southern Uplands, which lie south of the Southern Uplands Fault, are largely composed of Silurian deposits. The existing bedrock includes very ancient Archean gneiss, metamorphic beds interspersed with granite intrusions created during the Caledonian mountain building period (the Caledonian orogeny), commercially important coal, oil and iron bearing carboniferous deposits and the remains of substantial Palaeogene volcanoes. During their formation, tectonic movements created climatic conditions ranging from polar to desert to tropical and a resultant diversity of fossil remains. Scotland h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sutherland
Sutherland ( gd, Cataibh) is a historic county, registration county and lieutenancy area in the Highlands of Scotland. Its county town is Dornoch. Sutherland borders Caithness and Moray Firth to the east, Ross-shire and Cromartyshire (later combined into Ross and Cromarty) to the south and the Atlantic to the north and west. Like its southern neighbour Ross-shire, Sutherland has some of the most dramatic scenery in Europe, especially on its western fringe where the mountains meet the sea. These include high sea cliffs, and very old mountains composed of Precambrian and Cambrian rocks. The name ''Sutherland'' dates from the era of Norwegian Viking rule and settlement over much of the Highlands and Islands, under the rule of the jarl of Orkney. Although it contains some of the northernmost land in the island of Great Britain, it was called ' ("southern land") from the standpoint of Orkney and Caithness. In Gaelic, the area is referred to according to its traditional areas: ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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