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Gutland (Luxembourg)
Gutland (french: Bon Pays) is a region covering the southern and central parts of the Grand Duchy of Luxembourg. The Gutland (literally "Good Land") covers 68% of the territory of Luxembourg; to the north of Gutland lies the Oesling, which covers the remaining 32% of the Grand Duchy. To the east, the Luxembourgian Gutland adjoins the ''Bitburger Gutland'' of Germany. Gutland is not an homogeneous region, and includes five main sub-regions: the Valley of the Seven Castles, Little Switzerland, the Luxembourg plateau, the Moselle valley, and the Red Lands. Despite its variety, Gutland does have general geographic characteristics, both physical and human, that separate it from the Oesling. Unlike the sparsely populated Oesling, Gutland is relatively urbanised. Whereas the Oesling has only one town with a population larger than 2,000 people, Gutland has four cities with a population largely above 15,000 (Luxembourg City/LĂ«tzebuerg, Esch-sur-Alzette/Esch-Uelzecht, Differdange/DĂ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bech View 2011-08
Bech is a commune and small town in eastern Luxembourg. It is part of the canton of Echternach Echternach ( lb, Iechternach or (locally) ) is a commune with town status in the canton of Echternach, which is part of the district of Grevenmacher, in eastern Luxembourg. Echternach lies near the border with Germany, and is the oldest town in ..., which is part of the district of Grevenmacher. , the town of Bech, which lies in the east of the commune, has a population of 368. Villages within the commune include Altrier and Rippig. Population References External links * Towns in Luxembourg Communes in Echternach (canton) {{Echternach-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luxembourg (canton)
Luxembourg is a canton in the south of the Grand Duchy of Luxembourg. Its name, like the name of the Grand Duchy itself, derives from the name of its principal city, Luxembourg (more commonly known as Luxembourg City). It is not to be confused with the former district of Luxembourg, one of three administrative units in Luxembourg abolished in October 2015. It is the only canton, other than Mersch, to be entirely surrounded by other cantons and therefore to have no international boundary. Its capital is Luxembourg. Administrative divisions Luxembourg Canton consists of the following eleven communes: * Bertrange * Contern * Hesperange * Luxembourg * Niederanven * Sandweiler * Schuttrange * Steinsel * Strassen * Walferdange * Weiler-la-Tour Mergers * On 26 March 1920 the former communes of Hamm Hamm (, Latin: ''Hammona'') is a city in North Rhine-Westphalia, Germany. It is located in the northeastern part of the Ruhr area. As of 2016 its population was 179,397. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Luxembourg
In geography, regions, otherwise referred to as zones, lands or territories, are areas that are broadly divided by physical characteristics (physical geography), human impact characteristics (human geography), and the interaction of humanity and the environment (environmental geography). Geographic regions and sub-regions are mostly described by their imprecisely defined, and sometimes transitory boundaries, except in human geography, where jurisdiction areas such as national borders are defined in law. Apart from the global continental regions, there are also hydrospheric and atmospheric regions that cover the oceans, and discrete climates above the land and water masses of the planet. The land and water global regions are divided into subregions geographically bounded by large geological features that influence large-scale ecologies, such as plains and features. As a way of describing spatial areas, the concept of regions is important and widely used among the many branches of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral definin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as micas, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is usually given a name reflecting its protolith, such as ''schis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began domina ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of arch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esch-sur-Alzette (canton)
Esch-sur-Alzette is a canton in southwestern Luxembourg. Its capital is Esch-sur-Alzette. Administrative divisions Esch-sur-Alzette Canton consists of the following fourteen communes: * Bettembourg * Differdange * Dudelange * Esch-sur-Alzette * Frisange * Kayl * Leudelange * Mondercange * PĂ©tange PĂ©tange (; lb, PĂ©iteng, ; german: Petingen) is a commune and town in south-western Luxembourg. It is part of the canton of Esch-sur-Alzette. PĂ©tange lies on the borders with both Belgium and France. , the town of PĂ©tange, which lies in the ... * Reckange-sur-Mess * Roeser * Rumelange * Sanem * Schifflange Population References Cantons of Luxembourg {{Esch-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Duchy Of Luxembourg
Luxembourg ( ; lb, Lëtzebuerg ; french: link=no, Luxembourg; german: link=no, Luxemburg), officially the Grand Duchy of Luxembourg, ; french: link=no, Grand-Duché de Luxembourg ; german: link=no, Großherzogtum Luxemburg is a small landlocked country in Western Europe. It borders Belgium to the west and north, Germany to the east, and France to the south. Its capital and most populous city, Luxembourg, is one of the four institutional seats of the European Union (together with Brussels, Frankfurt, and Strasbourg) and the seat of several EU institutions, notably the Court of Justice of the European Union, the highest judicial authority. Luxembourg's culture, people, and languages are highly intertwined with its French and German neighbors; while Luxembourgish is legally the only national language of the Luxembourgish people, French and German are also used in administrative and judicial matters and all three are considered administrative languages of the country. With a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantons Of Luxembourg
The 12 cantons ( lb, Kantonen or ; french: cantons ; german: Kantone ) of the Grand Duchy of Luxembourg are areas of local government at the first level of local administrative unit (LAU-1) in the European Union's Nomenclature of Territorial Units for Statistics for Eurostat purposes. They were subdivisions of the three districts of Luxembourg until 2015, when the district level of government was abolished. The cantons are in turn subdivided into 102 communes An intentional community is a voluntary residential community which is designed to have a high degree of social cohesion and teamwork from the start. The members of an intentional community typically hold a common social, political, religious, ... (i.e. municipalities). List The following list gives the names of the cantons in French and Luxembourgish (in that order) which are both official languages of the Grand Duchy of Luxembourg: See also * :Lists of cantons of Luxembourg * ISO 3166-2:LU Referenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Red Lands
The Red Lands form a geographic region in southern and south-western Luxembourg. They are so called for their red iron-laden earth. The Red Lands roughly correspond with the southern part of the canton of Esch-sur-Alzette, along the border with France. Geologically, the Red Lands are sedimentary, mostly sandstones and conglomerates, formed in the Middle Jurassic epoch. As one of the most prodigious iron-producing regions in Western Europe, the Red Lands developed a thriving local steel industry, which has now developed into ArcelorMittal, the world's largest producer of steel. Throughout the period of industrial decline, the Red Lands have diversified into production of construction materials, engineering services, and chemical manufacturing. The region is the most densely populated part of Luxembourg, with several of Luxembourg's largest towns and cities, including Bettembourg, Differdange, Dudelange, Esch-sur-Alzette, Kayl, and Schifflange Schifflange ( lb, Schëffleng , german ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
