Achness Waterfall
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Achness Waterfall
Achness Falls, also known as the Achness Waterfall or Cassley Falls, is a waterfall located on the River Cassley in Sutherland, Scotland, near Rosehall and Invercassley. Its name is derived from the Scottish Gaelic ''Ach-an-eas'', the "field of the waterfall". The falls descend a narrow gorge with the upper fall being a drop. The lower fall is a thin broken sheet of water down about of rock and when in spate this becomes a torrent which has several pools providing a means for salmon to ascend. The location is the type locality and best-studied area of the Achness Thrust, a thrust fault which dips 40 to 50° to the south at the falls. Present nearby are the ruins of a broch and a more modern chapel. By the side of the river is an old cemetery and there are woodland walks. Atlantic salmon fishing on the River Cassley has a long history. Achness Falls is a temporary barrier to the fish each spring; they do not advance beyond it until the water warms above . In the late 19th cen ...
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Achness Water Falls On The River Cassley - Geograph
Achness Falls, also known as the Achness Waterfall or Cassley Falls, is a waterfall located on the River Cassley in Sutherland, Scotland, near Rosehall and Invercassley. Its name is derived from the Scottish Gaelic ''Ach-an-eas'', the "field of the waterfall". The falls descend a narrow gorge with the upper fall being a drop. The lower fall is a thin broken sheet of water down about of rock and when in spate this becomes a torrent which has several pools providing a means for salmon to ascend. The location is the type locality and best-studied area of the Achness Thrust, a thrust fault which dips 40 to 50° to the south at the falls. Present nearby are the ruins of a broch and a more modern chapel. By the side of the river is an old cemetery and there are woodland walks. Atlantic salmon fishing on the River Cassley has a long history. Achness Falls is a temporary barrier to the fish each spring; they do not advance beyond it until the water warms above . In the late 19th cen ...
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River Cassley
The River Cassley ( gd, Abhainn Charsla, ) in Sutherland, in northern Scotland, joins the River Oykel to form the Kyle of Sutherland at Invercassley (Inbhir Charsla). The Kyle is subsequently joined by the River Shin and River Carron (Abhainn Charrann) before it becomes the Dornoch Firth and enters the North Sea. The main road bridge over the river is at Rosehall, halfway between the mouth and the impressive Achness Waterfall Achness Falls, also known as the Achness Waterfall or Cassley Falls, is a waterfall located on the River Cassley in Sutherland, Scotland, near Rosehall and Invercassley. Its name is derived from the Scottish Gaelic ''Ach-an-eas'', the "field of ... or Cassley Falls. Like its more illustrious neighbour the Oykel, the Cassley is noted for its salmon and trout fishing. The lower river is in the same ownership as the Achaness Hotel at Rosehall, which provides accommodation and ghillies for visiting fishermen. Cassley {{Scotland-river-stub ...
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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: ' ...
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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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Rosehall
Rosehall is a remote hamlet in the Parish of Creich near the confluence of the River Cassley and the River Oykel, 1 mile northwest of Altass, in Sutherland, Scottish Highlands and is in the Scotland, Scottish council area of Highland Council area, Highland. It is the site of the main road bridge over the Cassley, which is just downstream from the spectacular Achness Waterfall, commonly known simply as the Cassley Falls. Amenities There is a hotel which caters mostly to visitors fishing for salmon in the two rivers. There are leisure trails across the Rosehall estate and a visitor cafe. Rosehall Estate Rosehall estate was the property of the Duke of Westminster until it was sold to become an hotel. The current house was built in 1873 after the original building was destroyed by fire. The Hugh Grosvenor, 2nd Duke of Westminster, second Duke entertained his lover Coco Chanel there. References

Populated places in Sutherland {{Highland-geo-stub ...
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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 ...
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Type Locality (geology)
Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified. If the stratigraphic unit in a locality is layered, it is called a stratotype, whereas the standard of reference for unlayered rocks is the type locality. The term is similar to the term type site in archaeology or the term type specimen in biology. Examples of geological type localities Rocks and minerals * Aragonite: Molina de Aragón, Guadalajara, Spain * Autunite: Autun, France * Benmoreite: Ben More (Mull), Scotland * Blairmorite: Blairmore, Alberta, Canada * Boninite: Bonin Islands, Japan * Comendite: Comende, San Pietro Island, Sardinia * Cummingtonite: Cummington, Massachusetts * Dunite: Dun Mountain, New Zealand. * Essexite: Essex County, Massachusetts, US * Fayalite: Horta, Fayal Island, Azores, Portugal * Harzburgite: Bad Harzburg, Germany * Icelandite: Thingmuli (Þingmúli), Iceland * Ijolite: Iivaara, Kuusamo, Finl ...
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Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular ''klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is referred to as a ''blind thrust'' fault. Because of the lack of surface evidence, blind thr ...
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Strike And Dip
Strike and dip is a measurement convention used to describe the orientation, or attitude, of a planar geologic feature. A feature's strike is the azimuth of an imagined horizontal line across the plane, and its dip is the angle of inclination measured downward from horizontal. They are used together to measure and document a structure's characteristics for study or for use on a geologic map. A feature's orientation can also be represented by dip and dip direction, using the azimuth of the dip rather than the strike value. Linear features are similarly measured with trend and plunge, where "trend" is analogous to dip direction and "plunge" is the dip angle. Strike and dip are measured using a compass and a clinometer. A compass is used to measure the feature's strike by holding the compass horizontally against the feature. A clinometer measures the features dip by recording the inclination perpendicular to the strike. These can be done separately, or together using a tool such a ...
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Broch
A broch is an Iron Age drystone hollow-walled structure found in Scotland. Brochs belong to the classification "complex Atlantic roundhouse" devised by Scottish archaeologists in the 1980s. Their origin is a matter of some controversy. Origin and definition The word ''broch'' is derived from Lowland Scots 'brough', meaning (among other things) fort. In the mid-19th century Scottish antiquaries called brochs 'burgs', after Old Norse ', with the same meaning. Place names in Scandinavian Scotland such as Burgawater and Burgan show that Old Norse ' is the older word used for these structures in the north. Brochs are often referred to as ''duns'' in the west. Antiquarians began to use the spelling ''broch'' in the 1870s. A precise definition for the word has proved elusive. Brochs are the most spectacular of a complex class of roundhouse buildings found throughout Atlantic Scotland. The Shetland Amenity Trust lists about 120 sites in Shetland as candidate brochs, while the Royal C ...
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Atlantic Salmon
The Atlantic salmon (''Salmo salar'') is a species of ray-finned fish in the family Salmonidae. It is the third largest of the Salmonidae, behind Siberian taimen and Pacific Chinook salmon, growing up to a meter in length. Atlantic salmon are found in the northern Atlantic Ocean and in rivers that flow into it. Most populations are anadromous, hatching in streams and rivers but moving out to sea as they grow where they mature, after which the adults seasonally move upstream again to spawn. When the mature fish re-enter rivers to spawn, they change in colour and appearance. Some populations of this fish only migrate to large lakes, and are "landlocked", spending their entire lives in freshwater. Such populations are found throughout the range of the species. Unlike Pacific species of salmon, ''S. salar'' is iteroparous, which means it can survive spawning and return to sea to repeat the process again in another year. Such individuals can grow to extremely large sizes, althoug ...
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