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Dale (landform)
A dale is a valley, especially an open, gently-sloping ground between low hills with a stream flowing through it. It is used most frequently in Northern England, the North of England and the Southern Uplands of Scotland; the term "fell" commonly refers to mountains or hills that flank a dale. As with many other words, ''dale'' was preserved by Danelaw, Viking influence in Northern England. It appears in various contexts, such as wikt:up_hill_and_down_dale, up hill and down dale "over every hill and dale", and "up all hills, down all dales. Etymology The word ''dale'' comes from the Old English word ''dæl'', from which the word "dell (landform), dell" also derived. It is related to Old Norse word ''dalr'' (and the modern Icelandic language, Icelandic word ''dalur'', etc.), which may have influenced its survival in northern England. The Germanic origin is assumed to be *''dala-''. ''Dal-'' in various combinations is common in placenames in Norway. Modern English valley and Frenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joachimsthaler
A thaler or taler ( ; , previously spelled ) is one of the large silver coins minted in the states and territories of the Holy Roman Empire and the Habsburg monarchy during the Early Modern period. A ''thaler'' size silver coin has a diameter of about and a weight of about 25 to 30 grams (roughly avoirdupois ounce, 1 ounce). The word is shortened from , the original ''thaler'' coin minted in Jáchymov, Joachimsthal, Kingdom of Bohemia, Bohemia, from 1520. While the first standard coin of the Holy Roman Empire was the of 1524, its longest-lived coin was the , which contained Cologne Mark of fine silver (or 25.984 g), and which was issued in various versions from 1566 to 1875. From the 17th century a lesser-valued ''North German thaler'' currency unit emerged, which by the 19th century became par with the . The ''thaler'' silver coin type continued to be minted until the 20th century in the form of the Mexican peso until 1914, the five Swiss franc coin until 1928, the US ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ennerdale, Cumbria
Ennerdale is a valley in Cumbria (in the former historic county of Cumberland), England. Ennerdale Water, fed by the River Liza, is the most westerly lake in the Lake District National Park. Due to the remote location, the lack of a public road up the valley, and its management by Forestry England, the National Trust and United Utilities, Ennerdale is relatively unspoiled. Ennerdale Water has not been as affected as other lakes in the National Park by construction, activity on the lake or the trappings of tourism. In 2022 the partners managing Ennerdale, together with Natural England, put together a successful proposal to declare much of the Ennerdale Valley as a National Nature Reserve (NNR). Environmental protection There are two biological Sites of Special Scientific Interest (SSSIs) in the valley: * Ennerdale * Pillar and Ennerdale Fells SSSI. Pillar and Ennerdale Fells is also protected as a Special Area of Conservation, being one of the ten SSSIs which underpin the Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coquetdale
The River Coquet runs through the county of Northumberland, England, discharging into the North Sea on the east coast at Amble. It rises in the Cheviot Hills on the border between England and Scotland, and follows a winding course across the landscape ("Coquetdale"). The upper reaches are bordered by the Otterburn Training Area, Otterburn Ranges military training ground, and are crossed by a number of bridges built in the 20th century. It passes a number of small villages and hamlets, and feeds one of the lakes created by extraction of gravel that form the Caistron Nature Reserve, before reaching the town of Rothbury, where it is crossed by a grade II listed bridge. Below the town is Thrum Mill, Rothbury, Thrum Mill, a Grade II-listed water mill. It loops around Brinkburn Priory, founded in the 1130s for Augustinians, Augustinian Canons, and its associated mill. At Felton, Northumberland, Felton it is crossed by two bridges, one dating from the 15th century, and its replacement ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Annandale, Dumfries And Galloway
Annandale is a district of Dumfriesshire, Scotland, centred on the dale or valley of the River Annan. It runs north–south through the Southern Uplands from Annanhead (north of Moffat) to Annan, Dumfries and Galloway, Annan on the Solway Firth. It is bordered by Nithsdale to the west and Eskdale, Scotland, Eskdale to the east. The Annandale Way runs the length of the valley, a distance of some . History Annandale is famous for its connection with Robert I of Scotland, Robert the Bruce, as the de Brus family was given this land by David I of Scotland, David I in 1124 as one of the border lordships when David became David, Prince of the Cumbrians, Prince of the Cumbrians. Along with Carrick, Scotland, Carrick, these lands acted as a buffer between the quasi-independent Lordship or Kingdom of Galloway and David's lands of Strathclyde and Cumbria. See also *Annandale distillery *Annadale, Shimla *Lord of Annandale, The Lordship of Annandale References External linksHistoric map ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Airedale
Airedale is a valley, or Dale (landform), dale, in North Yorkshire and West Yorkshire, England. It is named after the River Aire, which flows through it. The upper valley, from Malham Cove to Airton, is known as Malhamdale, named after the village of Malham. At Airton the valley widens and becomes Airedale proper. The river flows past Skipton on to Keighley, Bingley, Shipley, West Yorkshire, Shipley, and Leeds. Airedale, in conjunction with the Ribble Valley, provides low-altitude passes from Yorkshire to Lancashire through the Aire Gap. It is therefore an important transport route and was a strategically important area historically. History The upper Aire valley was formed 12,000 years ago by a retreating glacier. A moraine formed in the Cononley area and the lake stretched as far north as Gargrave. Colonisation by man developed later on, especially during the Iron Age. The peoples that occupied the Aire Valley (and much of north eastern England) were called Brigantes by t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dale (place Name Element)
A dale is a valley. It was commonly used in northern England and Scotland to denote an open valley as a dale, contrasted with a gill or narrow valley. List of places Places where dale is part of the name, but not the entire common name: United Kingdom England * Ainsdale, Merseyside * Allendale, Northumberland *Allerdale, Cumbria * Birkdale, Merseyside *Coalbrookdale, Shropshire *Derbyshire Dales **Darley Dale ** Glossopdale ** Lathkill Dale * Eskdale, Cumbria * Lonsdale, Lancashire and Cumbria * Redesdale, Northumberland *Rochdale, Greater Manchester * Rossendale, Lancashire *Skelmersdale, Lancashire *Yorkshire Dales **Airedale **Denby Dale ** Langstrothdale **Nidderdale **Ribblesdale ** Teesdale ** Wensleydale {{see also, List of Yorkshire Dales Scotland * Achrimsdale * Allandale * Allasdale *Armadale, Skye *Armadale, Sutherland * Annandale (other) * Arnisdale * Attadale * Bernisdale * Berriedale * Borrodale * Bracadale * Carradale * Cleadale * Clydesdale *Cromdale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thalweg
In geography, hydrography, and fluvial geomorphology, a thalweg or talweg () is the line or curve of lowest elevation within a valley or watercourse. Normally only the horizontal position of the curve is considered (as viewed on a map); the corresponding vertical position is represented in a '' stream profile''. Under international law, a thalweg is instead taken to be the middle of the primary navigable channel of a waterway which is the default legal presumption for the boundary between entities such as states. Thalwegs can have local proprietorial and administrative significance because their formerly somewhat shifting position, reliant on renewed soundings, now more fixed as described internationally, is part of centuries-old custom and practice in some jurisdictions. In some jurisdictions and between some states the median line (between banks) is the preferred boundary presumption as may extend from estuaries. Also being easy to map, drawing "turning points" are the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indo-European Languages
The Indo-European languages are a language family native to the northern Indian subcontinent, most of Europe, and the Iranian plateau with additional native branches found in regions such as Sri Lanka, the Maldives, parts of Central Asia (e.g., Tajikistan and Afghanistan), Armenia, and areas of southern India. Historically, Indo-European languages were also spoken in Anatolia. Some European languages of this family—English language, English, French language, French, Portuguese language, Portuguese, Russian language, Russian, Spanish language, Spanish, and Dutch language, Dutch—have expanded through colonialism in the modern period and are now spoken across several continents. The Indo-European family is divided into several branches or sub-families, including Albanian language, Albanian, Armenian language, Armenian, Balto-Slavic, Celtic languages, Celtic, Germanic languages, Germanic, Hellenic languages, Hellenic, Indo-Iranian languages, Indo-Iranian, and Italic languages, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Semantic Equivalency
{{about, semantic equivalence of metadata, the concept in mathematical logic, Logical equivalence, the concept in linguistic semantics, Semantic equivalence (linguistics) In computer metadata, semantic equivalence is a declaration that two data elements from different vocabularies contain data that has similar meaning. There are three types of semantic equivalence statements: * Class or concept equivalence. A statement that two high level concepts have similar or equivalent meaning. * Property or attribute equivalence. A statement that two properties, descriptors or attributes of classes have similar meaning. * Instance equivalence. A statement that two instances of data are the same or refer to the same instance. Example Assume that there are two organizations, each having a separate data dictionary. The first organization has a data element entry: PersonFamilyName The name of a person shared with other members of their family. and a second organization ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
