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Glen Ogle
Glen Ogle (Scottish Gaelic: Gleann Ogail) extends 7 miles north westwards from Lochearnhead to Lix Toll, where it opens into Glen Dochart. The Ogle Burn flows within the steep sides of the glen, from the Lochan Lairig Cheile at the glen's head. The military road, which can be seen from the modern road, was built in 1749 by Major William Caulfeild. It was used by the British Army in its efforts to pacify the Highlands after the Jacobite rising of 1745. Climate Glen Ogle has a subpolar oceanic climate (Köppen climate classification: Cfc), colder compared to most of the United Kingdom, which mostly features an oceanic climate (Köppen climate classification: Cfb). Railway walk It is possible to walk through the glen on a footpath that follows the course of the former Callander and Oban Railway to the summit of the glen and Killin Junction. The route uses the Category B listed long Glen Ogle viaduct, built between 1866 and 1870. The original design was for 20 arches, but the b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Ogle Viaduct
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' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scottish Gaelic
Scottish Gaelic ( gd, Gàidhlig ), also known as Scots Gaelic and Gaelic, is a Goidelic language (in the Celtic branch of the Indo-European language family) native to the Gaels of Scotland. As a Goidelic language, Scottish Gaelic, as well as both Irish and Manx, developed out of Old Irish. It became a distinct spoken language sometime in the 13th century in the Middle Irish period, although a common literary language was shared by the Gaels of both Ireland and Scotland until well into the 17th century. Most of modern Scotland was once Gaelic-speaking, as evidenced especially by Gaelic-language place names. In the 2011 census of Scotland, 57,375 people (1.1% of the Scottish population aged over 3 years old) reported being able to speak Gaelic, 1,275 fewer than in 2001. The highest percentages of Gaelic speakers were in the Outer Hebrides. Nevertheless, there is a language revival, and the number of speakers of the language under age 20 did not decrease between the 2001 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lochearnhead
Lochearnhead (Scottish Gaelic: Ceann Loch Èireann) is a village in Perthshire on the A84 Stirling to Crianlarich road at the foot of Glen Ogle, north of the Highland Boundary Fault. It is situated at the western end of Loch Earn where the A85 road from Crieff meets the A84. Loch Earn is above sea level, with the settlement running from its shores up to higher ground on the hills at the mouth of Glen Ogle. Lochearnhead lies within the Breadalbane area of the Loch Lomond and The Trossachs National Park. Early history The first evidence of people in Lochearnhead comes from Mesolithic arrowheads found in Glen Ogle by former local policeman Tom Gibbon, and his son Donald. A settled population is in evidence in the Neolithic period, from a burial chamber at Edinchip, and from the cup-marked stones which lie between the Kendrum Burn and the Craggan Road, in what is known locally as the Druid Field. There is another site with cup and ring marks at the head of Glen Ogle. There are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Dochart
Glen Dochart ( gd, Gleann Dochard) in Perthshire, Scottish Highlands is a glen which runs from Crianlarich eastwards to Killin, following the course of the River Dochart as it flows through Loch Dochart and Loch Iubhair. It is met by Glen Ogle ( gd, Gleann Ogail) at Lix Toll. Lochan Saorach lies within the glen and was once famous for its Floating island. Notable People *Rev Prof Daniel Dewar Daniel Dewar (1788–1867) was a Church of Scotland minister who served as principal of Marischal College in Aberdeen from 1832 to 1860. He was a major contributor to the first Gaelic dictionary. He was father-in-law to James Clerk Maxwell. Lif ... born and raised here References Glens of Scotland Valleys of Stirling (council area) {{Stirling-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Caulfeild (British Army Officer)
Major William Caulfeild was an officer in the British Army who is primarily known for his work supervising road and bridge construction in the Scottish Highlands in the 18th century. Early life He was born in Ireland, the son of the Hon. Toby Caulfeild who was a son of the first Viscount Charlemont. By the early 1730s, Caulfeild was serving as a Subaltern in the British Army. Roads and Bridges General Wade appointed him Inspector of Roads for Scotland in 1732. After the departure of General Wade in 1740, Caulfeild became responsible for directing all construction of new roads and bridges in Scotland until his death. Although he is not as well known as Wade, he is associated with the construction of far more roads than his predecessor. General Wade was responsible for of road, 40 bridges and 2 forts – whereas Caulfeild was responsible for of road and over 600 bridges. The largest individual lengths of roads built under the direction of Caulfeild included the military roads fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Army
The British Army is the principal land warfare force of the United Kingdom, a part of the British Armed Forces along with the Royal Navy and the Royal Air Force. , the British Army comprises 79,380 regular full-time personnel, 4,090 Gurkhas, and 28,330 volunteer reserve personnel. The modern British Army traces back to 1707, with antecedents in the English Army and Scots Army that were created during the Restoration in 1660. The term ''British Army'' was adopted in 1707 after the Acts of Union between England and Scotland. Members of the British Army swear allegiance to the monarch as their commander-in-chief, but the Bill of Rights of 1689 and Claim of Right Act 1689 require parliamentary consent for the Crown to maintain a peacetime standing army. Therefore, Parliament approves the army by passing an Armed Forces Act at least once every five years. The army is administered by the Ministry of Defence and commanded by the Chief of the General Staff. The Brit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jacobite Rising Of 1745
The Jacobite rising of 1745, also known as the Forty-five Rebellion or simply the '45 ( gd, Bliadhna Theàrlaich, , ), was an attempt by Charles Edward Stuart to regain the Monarchy of Great Britain, British throne for his father, James Francis Edward Stuart. It took place during the War of the Austrian Succession, when the bulk of the British Army was fighting in mainland Europe, and proved to be the last in Jacobite risings, a series of revolts that began in Jacobite rising of 1689, 1689, with major outbreaks in 1708, Jacobite rising of 1715, 1715 and Jacobite rising of 1719, 1719. Charles launched the rebellion on 19 August 1745 at Glenfinnan in the Scottish Highlands, capturing Edinburgh and winning the Battle of Prestonpans in September. At a council in October, the Scots agreed to invade England after Charles assured them of substantial support from English Jacobitism, Jacobites and a simultaneous French landing in Southern England. On that basis, the Jacobite Army (1745) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subpolar Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Callander And Oban Railway
The Callander and Oban Railway company was established with the intention of linking the sea port of Oban to the railway network. This involved a long line from Callander through wild and thinly populated terrain, and shortage of money meant that the line was opened in stages from 1866 to 1880. The line improved the economy of Oban, especially for the fishing trade and for tourism, but the winter traffic was limited. The company built a branch to Ballachulish, which included the construction of Connel Bridge, a remarkable bridge at Connel over Loch Etive. The branch opened in 1903, but although it opened up remote areas it was never commercially successful. It closed in 1966. The main line was crossed by the West Highland Line at Crianlarich, where a connecting spur was constructed by the West Highland Line in 1897. The C&OR section between Callander and Crianlarich was closed in September 1965. However, the section between Crianlarich and Oban is still in use today, with trains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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