Strathdevon
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Strathdevon
Strathdevon is the strath of the River Devon in Clackmannanshire, Scotland. Strathdevon is associated with the parish of Muckhart and was up until 1971 the southernmost tip of Perthshire. The strath stretches east to west from upper Yetts o' Muckhart and the Glen Devon area westwards along the Ochil Hills. Strathdevon includes the settlements of Muckhart, Dollar, Tillicoultry, Alva and Menstrie on the A91, and Rumbling Bridge. In the upper Yetts o' Muckhart there is a building that was the turnpike for the B934 road that leads to Dunning Glen and the A823, which in turn leads to Glen Devon and Gleneagles. Geography The Strathdevon and Crook of Devon areas of Perth and Kinross, in which the River Devon and Black Devon flow, are overlooked by the tops of the Ochil Hills, from where most of the area can be seen. The Black Devon flows past Clackmannan and links with the River Forth south of Alloa. The Ochil Hills supply the water that Highland Spring sells worldwid ...
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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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Tillicoultry
Tillicoultry ( ; Scottish Gaelic: Tulach Cultraidh, perhaps from older Gaelic ''Tullich-cul-tir'', or "the mount/hill at the back of the country") is a town in Clackmannanshire, Scotland. Tillicoultry is usually referred to as Tilly by the locals. One of the Hillfoots Villages on the A91, which runs from Stirling to St. Andrews, Tillicoultry is situated at the southern base of the Ochil Hills, which provide a spectacular backdrop. The River Devon, Scotland, River Devon lies to the south. The river also runs through neighbouring villages Dollar, Clackmannanshire, Dollar and Alva, Scotland, Alva to the east and west respectively. The former Pit village, mining village of Coalsnaughton lies just south, whilst Alloa lies southwest. The "hill" referred to in the first etymology is likely to be Kirkhill, at the east of the town. The alternative Latin etymology, ''Tellus culta'', the cultivated land, suggested by Rev. William Osborne, minister of the parish from 1773 to 1794, is als ...
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Strath
A strath is a large valley, typically a river valley that is wide and shallow (as opposed to a glen, which is typically narrower and deep). Word and etymology An anglicisation of the Gaelic word ''srath'', it is one of many that have been absorbed into the English and Scots languages. It is commonly used in rural Scotland to describe a wide valley, even by non-Gaelic speakers. In Scottish place-names, ''Strath-'' is of Gaelic and Brittonic origin. ''Strath-'' names have the genesis with Gaelic ''srath'' meaning "broad-valley", as well as with the Cumbric and Pictish cognates (c.f. Welsh ''ystrad''). Gaelic ''srath'' is derived from Old Irish ''srath'', recorded as having meant "grassland". The modern Scottish Gaelic sense of "broad-valley", paralleling the meaning of Brittonic cognates, developed from substrate influence from Pictish. Toponymy It occurs in numerous place names within Scotland including Strathspey and Strathclyde. Internationally, many places with Scott ...
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Black Devon
The Black Devon is a river in Scotland. It rises in the Cleish Hills, specifically the area known as Outh Muir, north of Knockhill Racing Circuit, around north-west of Dunfermline, Fife, with the gathering of three small streams in branch formation. The river flows westwards through Balgonar, north of Saline, and then merges with the Saline Burn. The Black Devon flows into Clackmannanshire, through the hamlet of Forestmill and past the town of Clackmannan. The Black Devon enters the River Forth south of Alloa, north of Dunmore Pier. It is a narrow and shallow river that holds wild brown trout, and also sees sea trout in winter months that come into the Firth of Forth, which is tidal as far as Stirling. The Rivers and Fisheries Trusts of Scotland manage the River Forth and its tributary rivers, which besides the Black Devon include the River Devon, River Teith, and River Allan. Disappearance In June 1952 the last two miles of the Black Devon disappeared into old coal min ...
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Sea Trout
Sea trout is the common name usually applied to anadromous (sea-run) forms of brown trout (''Salmo trutta''), and is often referred to as ''Salmo trutta'' morpha ''trutta''. Other names for anadromous brown trout are sewin (Wales), peel or peal ( Southwest England), mort (Northwest England), finnock (Scotland), white trout (Ireland) and salmon trout (culinary). The term "sea trout" is also used to describe other anadromous salmonids, such as coho salmon (''Oncorhynchus kisutch''), coastal cutthroat trout (''Oncorhynchus clarkii clarkii''), brook trout (''Salvelinus fontinalis''), Arctic char (''Salvelinus alpinus alpinus'') and Dolly Varden (''Salvenlinus malma''). Even some non-salmonid fish species are also commonly known as sea trout, such as Northern pikeminnow (''Ptychocheilus oregonensis'') and members of the weakfish family (''Cynoscion''). Range Anadromous brown trout are widely distributed in Europe along the Atlantic and Baltic coasts, the United Kingdom and the coa ...
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Salmon
Salmon () is the common name for several list of commercially important fish species, commercially important species of euryhaline ray-finned fish from the family (biology), family Salmonidae, which are native to tributary, tributaries of the North Atlantic (genus ''Salmo'') and North Pacific (genus ''Oncorhynchus'') basin. Other closely related fish in the same family include trout, Salvelinus, char, Thymallus, grayling, Freshwater whitefish, whitefish, lenok and Hucho, taimen. Salmon are typically fish migration, anadromous: they hatch in the gravel stream bed, beds of shallow fresh water streams, migrate to the ocean as adults and live like sea fish, then return to fresh water to reproduce. However, populations of several species are restricted to fresh water throughout their lives. Folklore has it that the fish return to the exact spot where they hatched to spawn (biology), spawn, and tracking studies have shown this to be mostly true. A portion of a returning salmon run ma ...
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European Otter
The Eurasian otter (''Lutra lutra''), also known as the European otter, Eurasian river otter, common otter, and Old World otter, is a semiaquatic mammal native to Eurasia. The most widely distributed member of the otter subfamily (Lutrinae) of the weasel family (Mustelidae), it is found in the waterways and coasts of Europe, many parts of Asia, and parts of northern Africa. The Eurasian otter has a diet mainly of fish, and is strongly territorial. It is endangered in some parts of its range, but is recovering in others. Description The Eurasian otter is a typical species of the otter subfamily. Brown above and cream below, these long, slender creatures are well-equipped for their aquatic habits. Their bones show osteosclerosis, increasing their density to reduce buoyancy. This otter differs from the North American river otter by its shorter neck, broader visage, the greater space between the ears and its longer tail. However, the Eurasian otter is the only otter in much of its r ...
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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ...
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Cobalt
Cobalt is a chemical element with the symbol Co and atomic number 27. As with nickel, cobalt is found in the Earth's crust only in a chemically combined form, save for small deposits found in alloys of natural meteoric iron. The free element, produced by reductive smelting, is a hard, lustrous, silver-gray metal. Cobalt-based blue pigments ( cobalt blue) have been used since ancient times for jewelry and paints, and to impart a distinctive blue tint to glass, but the color was for a long time thought to be due to the known metal bismuth. Miners had long used the name ''kobold ore'' (German for ''goblin ore'') for some of the blue-pigment-producing minerals; they were so named because they were poor in known metals, and gave poisonous arsenic-containing fumes when smelted. In 1735, such ores were found to be reducible to a new metal (the first discovered since ancient times), and this was ultimately named for the ''kobold''. Today, some cobalt is produced specifically from one of ...
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Silver
Silver is a chemical element with the Symbol (chemistry), symbol Ag (from the Latin ', derived from the Proto-Indo-European wikt:Reconstruction:Proto-Indo-European/h₂erǵ-, ''h₂erǵ'': "shiny" or "white") and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical conductivity, thermal conductivity, and reflectivity of any metal. The metal is found in the Earth's crust in the pure, free elemental form ("native silver"), as an alloy with gold and other metals, and in minerals such as argentite and chlorargyrite. Most silver is produced as a byproduct of copper, gold, lead, and zinc Refining (metallurgy), refining. Silver has long been valued as a precious metal. Silver metal is used in many bullion coins, sometimes bimetallism, alongside gold: while it is more abundant than gold, it is much less abundant as a native metal. Its purity is typically measured on a per-mille basis; a 94%-pure alloy is described as "0.940 fine". As one of th ...
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Gold
Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile metal in a pure form. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements and is solid under standard conditions. Gold often occurs in free elemental ( native state), as nuggets or grains, in rocks, veins, and alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum), naturally alloyed with other metals like copper and palladium, and mineral inclusions such as within pyrite. Less commonly, it occurs in minerals as gold compounds, often with tellurium (gold tellurides). Gold is resistant to most acids, though it does dissolve in aqua regia (a mixture of nitric acid and hydrochloric acid), forming a soluble tetrachloroaurate anion. Gold is ...
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