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Forth Valley
The River Forth is a major river in central Scotland, long, which drains into the North Sea on the east coast of the country. Its drainage basin covers much of Stirlingshire in Scotland's Central Belt. The Gaelic name for the upper reach of the river, above Stirling, is ''Abhainn Dubh'', meaning "black river". The name for the river below the tidal reach (just past where it is crossed by the M9 motorway) is ''Uisge For''. Name ''Forth'' derives from Proto-Celtic ''*Vo-rit-ia'' (slow running), yielding '' Foirthe'' in Old Gaelic. Course The Forth rises in the Trossachs, a mountainous area west of Stirling. Ben Lomond's eastern slopes drain into the Duchray Water, which meets with Avondhu River coming from Loch Ard. The confluence of these two streams is the nominal start of the River Forth. From there it flows roughly eastward through Aberfoyle, joining with the Kelty Water about 5 km further downstream. It then flows into the flat expanse of the Carse of Stirling, i ...
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Scotland
Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast and east, and the Irish Sea to the south. It also contains more than 790 islands, principally in the archipelagos of the Hebrides and the Northern Isles. Most of the population, including the capital Edinburgh, is concentrated in the Central Belt—the plain between the Scottish Highlands and the Southern Uplands—in the Scottish Lowlands. Scotland is divided into 32 administrative subdivisions or local authorities, known as council areas. Glasgow City is the largest council area in terms of population, with Highland being the largest in terms of area. Limited self-governing power, covering matters such as education, social services and roads and transportation, is devolved from the Scott ...
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Carse
In Scottish geography, a Carse (the modern form of older Scots ; Scottish Gaelic or ) is an area of fertile, low-lying (typically alluvial) land occupying certain Scottish river valleys, such as that of the River Forth. Carse of Forth The Carse of Forth contrasts with the Ochil Hills to the north, from which it is separated by the Ochil Fault. The carse is generally so flat that, except in the case of alluvial fans, such as that on which the small town of Alva is situated, it has only reached a height of about 9 metres above sea level at the Ochil Fault, typically two or more miles from the river. In the case of the River Forth, the carse extends some considerable distance above and below Stirling, where due to constraints such as the Abbey Craig to the north and the castle rock, on which the town is based, to the south, it is very narrow. The carse typically offers good agricultural land, however underlying the topsoil and alluvium is glacial boulder clay. In other places ...
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Clackmannanshire
Clackmannanshire (; sco, Clackmannanshire; gd, Siorrachd Chlach Mhannainn) is a historic county, council area, registration county and Lieutenancy area in Scotland, bordering the council areas of Stirling, Fife, and Perth & Kinross and the historic counties of Perthshire, Stirlingshire and Fife. The name consists of elements from three languages. The first element is from gd, Clach meaning "Stone". Mannan is a derivative of the Brythonic name of the Manaw, the Iron Age tribe who inhabited the area. The final element is the English word shire. As Britain's smallest historic county, it is often nicknamed "The Wee County". When written, Clackmannanshire is commonly abbreviated to Clacks. History Clackmannan, the old county town, is named after the ancient stone associated with the pre-Christian deity Manau or Mannan. The stone now rests on a larger stone beside the Tollbooth (built late 16th century) and Mercat Cross at the top of Main street, Clackmannan. Clackmannanshire ...
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Fallin, Stirling
Fallin () is a village in the Stirling council area of Scotland. It lies on the A905 road 3 miles east of Stirling on a bend in the River Forth. The United Kingdom Census 2001 recorded the population as 2,710. It was formerly a pit village, the site of the Polmaise Colliery 3&4 (Polmaise Colliery 1&2 was situated at Milhall), originally opened in 1904 by Archibald Russell Ltd. At its peak, in 1957, it employed 778 people. During the UK miners' strike 1984-85 The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Europe, off the north-western coast of the continental mainland. It comprises England, Scotland, Wales and North ... it was reputed to be the only colliery in Britain where support was so strong that there was no need for pickets during the whole of the strike. British Coal decided to close the Colliery on 17 July 1987, marking the end of coal mining in Stirlingshire. The village is h ...
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Bannock Burn
The Bannock Burn ( gd, Allt a' Bhonnaich) is a stream (''burn'' is Scots for stream) which rises at about 1,300 feet on Touchadam Moor, NS715891, just to the north of Earl's Hill in the Touch Hills to the south-west of Stirling in central Scotland. The Bannock flows eastward and enters the River Forth to the east of Stirling, close to the site of the Battle of Bannockburn (1314), about 7.58 miles from its source. The burn itself meanders and is considerably longer. A nearby town, nowadays a suburb of Stirling, is accordingly called Bannockburn. The Battle of Sauchieburn (1488) was also fought close to the Bannock Burn. Early Habitation The upper part of the valley of the Bannock Burn appears to have been inhabited in the Iron Age. Several duns are to be found in the Graigend and Murrayshall area and a fort on Lewis Hill. The Dun at Wallstale (NS774909) was partly excavated in June 1965.. A trench was cut across the line of the wall and into the interior, revealing that the w ...
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Ford (river)
A ford is a shallow place with good footing where a river or stream may be crossed by wading, or inside a vehicle getting its wheels wet. A ford may occur naturally or be constructed. Fords may be impassable during high water. A low-water crossing is a low bridge that allows crossing over a river or stream when water is low but may be treated as a ford when the river is high and water covers the crossing. Description A ford is a much cheaper form of river crossing than a bridge, and it can transport much more weight than a bridge, but it may become impassable after heavy rain or during flood conditions. A ford is therefore normally only suitable for very minor roads (and for paths intended for walkers and horse riders etc.). Most modern fords are usually shallow enough to be crossed by cars and other wheeled or tracked vehicles (a process known as "fording"). Fords may be accompanied by stepping stones for pedestrians. The United Kingdom has more than 2,000 fords, and most o ...
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Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravity, gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the #Phase and amplitude, phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see ''#Timing, Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal cycle, diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude ...
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Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ...
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Allan Water
The Allan Water ( gd, Uisge Alain) is a river in central Scotland. Rising in the Ochil Hills, it runs through Strathallan to Dunblane and Bridge of Allan before joining the River Forth. It is liable to cause floods in lower Bridge of Allan. It shares its name with a tributary of the River Teviot. The name is similar to the Ale Water in Berwickshire, the River Alness in Ross-shire, the Allander Water in Stirlingshire, the River Alne and the Ayle Burn in Northumberland, the River Ellen in Cumbria, and several names in the south of England, Wales and Cornwall. Ptolemy, who wrote his Geography about 150 AD, gave the names of some of these rivers as Alauna or Alaunos. Ekwall says that Alauna or Alaunos are British .e. Brythonic or P-Celticriver names. Nicolaisen says that the name Allan is of Pre-Celtic Indo-European origin. Its original form was Alauna, from the Indo-European root *el-/ol-, meaning "to flow, to stream". Several European rivers and settlements have names that may ...
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Loch Voil
Loch Voil ( gd, Loch a' Bheothail) is a small freshwater loch that lies to the west of Balquhidder in the Stirling council area of Scotland. It is a short, narrow loch. It is separated from Loch Doine by fluvial deposits from the Monachyle Burn and is drained at its eastern end by the River Balvag at Balquhidder. The Loch can be reached by a small single track road from Balquhidder Balquhidder (; gd, Both Chuidir or ) is a small village in Perthshire located north-west of Callander. It is administered by the Stirling council area of Scotland and is overlooked by the dramatic mountain terrain of the 'Braes of Balquhidde ... leading to Inverlochlarig. References {{Commons category Voil Voil LVoil ...
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Loch Katrine
Loch Katrine (; or ) is a freshwater loch in the Trossachs area of the Scottish Highlands, east of Loch Lomond, within the historic county and registration county of Perthshire and the contemporary district of Stirling. The loch is about long and wide at its widest point, and runs the length of Strath Gartney (Gaelic: ''Srath Ghartain''). It is within the drainage basins of the River Teith and River Forth. It is a popular scenic attraction for tourists and day-visitors from Glasgow and nearby towns; fly and boat fishing for trout are permitted on the loch from spring to autumn. It also serves as a reservoir for the water supply of the Glasgow conurbation, some south, being connected by two aqueducts constructed in 1859. It is the fictional setting of Sir Walter Scott's poem ''The Lady of the Lake'' and of the subsequent opera by Gioachino Rossini, ''La donna del lago''. Name etymology William Watson, a renowned scholar of Scottish place names, judged ''Katrine'' to be "t ...
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Loch Lubnaig
Loch Lubnaig (Loch Lùbnaig in Gaelic) is a small freshwater loch near Callander in the Stirling council area, Scottish Highlands. It lies in the former county of Perthshire. It is part of the Loch Lomond and The Trossachs National Park. The loch nestles in the space between Ben Ledi and Ben Vorlich. Fed by the River Balvaig from the north and drained by the Garbh Uisge to the south, Loch Lubnaig offers fishing from the shore while canoes can be rented at the north end. Alternatively, two car parking areas on the east shore offer perfect, albeit sometimes busy, canoe launching points. The route of the former Callander and Oban Railway runs along the west shore of the loch. This route has now been converted to a part of the National Cycle Network's "Route 7" allowing cyclists and walkers to travel the between Callander and Strathyre. The name is derived from the Gaelic Lùbnaig, meaning ''crooked''. Like many lochs of the Highlands, the name is almost identical to its Gaelic ...
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