River Garry, Perthshire
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River Garry, Perthshire
The River Garry ( gd, Gar / Abhainn Ghar) is a major tributary of the River Tummel, itself a tributary of the River Tay, in the traditional county of Perthshire in the Scottish Highlands. It emerges from the northeastern end of Loch Garry just to the southeast of the Pass of Drumochter, and flows southeastwards and eastwards down Glen Garry to the narrow Pass of Killiecrankie beyond which it joins the Tummel Loch Garry itself is fed by the Allt Shallainn, Allt na Duinish and Allt na Cosaig which enter its southern end. The loch occupies a deep northeast-southwest aligned trench cut by glacial action. Glen Garry provides the main route northwards for both the A9 road and the railway from Perth to Inverness. Tributaries The principal tributaries of the Garry are the Allt Dubhaig, Edendon Water, Errochty Water, Bruar Water and the River Tilt. Arising in the Dalnaspidal Forest, the Allt Dubhaig joins the Garry near Dalnaspidal Lodge at the southern end of the Pass of Drumocht ...
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River Garry At Dalnacardoch
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, sprin ...
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Trinafour
Trinafour (; gd, Trian a' Phùir) is a village in Perth and Kinross, Scotland, approximately north-west of Pitlochry Pitlochry (; gd, Baile Chloichridh or ) is a town in the Perth and Kinross council area of Scotland, lying on the River Tummel. It is historically in the county of Perthshire, and has a population of 2,776, according to the 2011 census.Scotla ..., its nearest town. It is located at the western edge of Glen Errochty. References External links Trinafour at AboutBritain.com Villages in Perth and Kinross {{PerthKinross-geo-stub ...
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Loch Loch
Loch Loch is a remote freshwater loch, located in Glen Loch in Perth and Kinross, some 9.5 miles north of Pitlochry, Scotland and is within the ''Forest of Atholl''. Geography Loch Loch is situated in wild mountainous scenery and is located with hills on both sides that have very steep sides. Beinn a' Ghlò is situated to the west side and the precipitous crags of Craig an loch in the east. Mounds of gravelly moraine A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice shee ... form the greater part of both shores, forming the prominent points. The loch flows northward by the An Lochain into the River Tilt, which also receives the water of Loch Tilt at the head of the glen. The loch is on a north to south bearing, and is long and narrow loch, or rather two lochs as there is a narrow con ...
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Falls Of Tarf
The Falls of Tarf is a waterfall on the Tarf Water in the eastern Highlands of Scotland. Immediately downstream of the falls the Tarf is joined by a second, smaller river to become the River Tilt.Ordnance Survey 1:25,000 scale Explorer map series, sheets 309-470 See also *Waterfalls of Scotland Much of Scotland is mountainous; western areas of the Highlands enjoy a wet climate. The more steeply plunging west coast highland rivers in particular are home to countless waterfalls. Scotland has over 150 waterfalls, most are situated in the Hi ... References Waterfalls of Perth and Kinross {{Scotland-geo-stub ...
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Blair Atholl
Blair Atholl (from the Scottish Gaelic: ''Blàr Athall'', originally ''Blàr Ath Fhodla'') is a village in Perthshire, Scotland, built about the confluence of the Rivers Tilt and Garry in one of the few areas of flat land in the midst of the Grampian Mountains. The Gaelic place-name Blair, from ''blàr'', 'field, plain', refers to this location. Atholl, which means 'new Ireland', from the archaic ''Ath Fhodla'' is the name of the surrounding district. On 13 March 2008, it was announced that Blair Atholl (together with some other Highland Perthshire villages) would be included in the Cairngorms National Park. This change was made at the request of the people of the town. The Forest of Atholl already formed part of the Cairngorms. Blair Castle Blair Atholl's most famous feature is Blair Castle (NN 865 662), one of Scotland's premier stately homes, and the last castle in the British Isles to be besieged, in 1746 during the last Jacobite rising. The Castle was the traditional ...
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Glen Tilt
Glen Tilt (Scottish Gaelic: Gleann Teilt) is a glen in the extreme north of Perthshire, Scotland. Beginning at the confines of Aberdeenshire, it follows a South-westerly direction excepting for the last 4 miles, when it runs due south to Blair Atholl. It is watered throughout by the Tilt, which enters the Garry after a course of 14 miles, and receives on its right the Tarf, which forms some beautiful falls just above the confluence, and on the left the Fender, which has some fine falls also. The attempt of George Murray, 6th Duke of Atholl to close the glen to the public was successfully contested by the Scottish Rights of Way Society in 1847. The massive mountain of Beinn a' Ghlò and its three Munros Càrn nan Gabhar (1129 m), Bràigh Coire Chruinn-bhalgain (1070 m) and Càrn Liath (975) dominate the glen's eastern lower half. Marble of good quality is occasionally quarried in the glen, and the rock formation has long attracted the attention of geologists. One of the earliest ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Falls Of Bruar
The Falls of Bruar are a series of waterfalls on the Bruar Water in Scotland, about from Pitlochry in the council area of Perth and Kinross. They have been a tourist attraction since the 18th century and were immortalized in a poem by Robert Burns, ''The Humble Petition of Bruar Water to the Noble Duke of Atholl'', supposedly from the river itself entreating the Duke to plant some trees in the then barren landscape. Description The falls were probably formed some time in the last 10,000 years, after the retreat of the glaciers at the end of the last ice age. The waters slowly cut through the rock which had been pushed up by the geological forces which formed the Scottish Highlands some 500 million years ago. The layering of the rocks means that the water has cut a meandering path through the softer rock and left the harder rock untouched. This has led to the creation of deep pools, outcrops and, in one place, a natural arch. The falls consist of two large falls and a number of s ...
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Calvine
Calvine is a hamlet in Perth and Kinross, Scotland. It is sandwiched between the A9 road, to its north, and the Highland mainline railway and River Garry, both to its south, and lies just north of Struan and west of Pitagowan. The Falls of Bruar The Falls of Bruar are a series of waterfalls on the Bruar Water in Scotland, about from Pitlochry in the council area of Perth and Kinross. They have been a tourist attraction since the 18th century and were immortalized in a poem by Robert Bu ... are one mile to the south-west. The former route of the A9, now the B847, runs through the settlement. The hamlet is known for the Calvine UFO sighting, which occurred nearby, in 1990. References Villages in Perth and Kinross {{PerthKinross-geo-stub ...
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Loch Errochty
Loch Errochty is a man made freshwater loch situated within the Perth and Kinross council area at the edge of the Scottish Highlands near the Highland Boundary Fault where the topography changes to lowland. Overview The Errochty dam lies at the head of Glen Errochty, two km NW of the hamlet of Trinafour at the approximate grid reference of . The loch has an area of 303 hectareswww.almanacofscotland.co.uk.
Gives surface area of loch.
and is 5 km long and a kilometre across at its widest point. The loch is entirely man made, being created by the damming of the Errochty Water, the river which runs down the glen. The dam was constructed in 1957 by the contractors A. & M. Carmichael Ltd as part of phase two of the

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Deer Forest
The deer forest (Gaelic: frìth) is a sporting estate which is kept and managed largely or solely for the purposes of maintaining a resident population of red deer for sporting (deer stalking) purposes. It is an institution and phenomenon peculiar to the Highlands of Scotland. Typically, deer forests are in hilly and mountainous areas of the Highlands and Islands; and, despite the use of the term "forest" they are almost all devoid of trees - the word is used here in its original sense, meaning an area set aside for hunting, rather than its later association with trees (see Royal Forest). The land is typically not suitable for crops. Most deer forests have large areas covered with heath, in many places peat bogs, marshes, lochs or bare rock, elsewhere patches of grass or other herbage, while plantations of trees of greater or less extent may also occur. They usually extend to and more, and deer which live there belong to the small-bodied, hill-dwelling race of red deer typical ...
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