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Geisberg (Middle Moselle)
{{Infobox mountain , name = Geisberg , other_name = Bitschberg, Pitsch Berg, Bitsch, Benhaar, Geischberg , etymology = , native_name = , native_name_lang = , translation = , pronunciation = , photo = Goldener Oktober 2016 Geisberg.jpg , photo_size = , photo_alt = , photo_caption = The Geisberg (literally: Goats Hill) seen from the north-west, Moselle in between, Mühlheim village to the left , map = , map_image = , map_alt = , map_caption = , map_relief = , map_size = , location = , label = , label_position = , elevation = , elevation_m = 262 , elevation_ft = , elevation_ref = , prominence = , prominence_m = , prominence_ft = , prominence_ref = , isolation = , isolation_km = , isolation_mi = , isolation_ref = , ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Region
A natural region (landscape unit) is a basic geographic unit. Usually, it is a region which is distinguished by its common natural features of geography, geology, and climate. From the ecology, ecological point of view, the naturally occurring flora and fauna of the region are likely to be influenced by its geographical and geological factors, such as soil and water resources, water availability, in a significant manner. Thus most natural regions are homogeneous ecosystems. Human impact can be an important factor in the shaping and destiny of a particular natural region. Main terms The concept "natural region" is a large basic geographical unit, like the vast boreal forest region. The term may also be used generically, like in alpine tundra, or specifically to refer to a particular place. The term is particularly useful where there is no corresponding or coterminous official region. The Fens of eastern England, the Thai highlands, and the Pays de Bray in Normandy, are examples o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burgen (bei Bernkastel-Kues)
Burgen is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany. Geography Location The municipality lies at the outermost end of an ancient river valley of the Middle Moselle, which formed at a time when the river had not settled on the course that it now follows. Burgen is found right below the Hunsrück’s first forests and from the point of view of transport, lies on a dead end. However, it can be reached from two directions, from Brauneberg over ''Kreisstraße'' 87 and from Veldenz over ''Kreisstraße'' 89. South of the municipality is only Brauneberg’s outlying centre of Hirzlei, where ''Kreisstraße'' 87 comes to an end. There is almost no through traffic. Burgen belongs to the ''Verbandsgemeinde'' of Bernkastel-Kues, whose seat is in the like-named town. Nearby communities Neighbouring municipalities are, among others, Brauneberg with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lieser, Germany
Lieser () is an ''Ortsgemeinde'' – a Municipalities of Germany, municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Bernkastel-Wittlich Districts of Germany, district in Rhineland-Palatinate, Germany. Geography Location Lieser belongs to the Bernkastel-Kues (Verbandsgemeinde), ''Verbandsgemeinde'' of Bernkastel-Kues, whose seat is in the Bernkastel-Kues, like-named town. It lies on the Middle Moselle (river), Moselle and is named after the river Lieserbach, which empties into the Moselle west of Lieser. The village is shaped like an upside-down T (when viewed from the south) as many houses have been built below the vineyards, along the Moselle's bank. The older part of the lower village exhibits tight Terraced house, terraced housing development with vineyards lying behind, owing to the intensive winegrowing. Rising up over the village is the Baroque architecture, Late Baroque Saint Peter's Parish Church (''Pfarrkirche St. Peter'') ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wittlich Depression
The Wittlich Depression (german: Wittlicher Senke or ''Wittlicher Rotliegend-Senke''), less commonly, the Wittlich Basin, is the continuation of the Trier Valley in a northeasterly direction. It is not only recognisable in the terrain as an elongated depression, but also from its geological structure as a basin. From a natural region perspective, the Wittlich Depression (252) is one of three major units of the Moselle Valley major unit group Moseltal (25). The ''Wittlich Depression Cycleway'' (''Radweg Wittlicher Senke'') runs through the region. Geography The Wittlich Depression runs for about 45 kilometres from Schweich in the southwest almost to the River Moselle northeast of Wittlich. At its widest point it is about 7 kilometres across. Its average height is about , its lowest point is near Wengerohr in the vicinity of Wittlich and on the Lieser, a tributary of the Moselle in Rhineland-Palatinate. The depression is bounded to the northwest by the Meulenwald fore ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osann-Monzel
Osann-Monzel is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – and a winegrowing centre in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany. Geography Location The municipality lies on the Middle Moselle on a slope set two kilometres back from the river, between the two hills of Hüttenkopf and Rosenberg in a side valley through which a bend in the Moselle flowed in the Tertiary. Osann-Monzel's elevation is some 180 m above sea level. Osann-Monzel belongs to the ''Verbandsgemeinde'' of Wittlich-Land, whose seat is in Wittlich, although that town is itself not part of the ''Verbandsgemeinde''. Constituent communities Osann-Monzel's ''Ortsteile'' are, as the name suggests, Osann and Monzel. They were merged to form today's municipality in 1969. History The Osann-Monzel area is believed to have first been settled in Roman times after Julius Caesar (100 BC – 44 BC) had abs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dietrich 1910 Abb 2 Alte Flussläufe Ausschnitt En
Dietrich () is an ancient German name meaning "Ruler of the People.” Also "keeper of the keys" or a "lockpick" either the tool or the profession. Given name * Dietrich, Count of Oldenburg (c. 1398 – 1440) * Thierry of Alsace (german: Dietrich, link=no; 1099–1168), Count of Flanders * Dietrich of Ringelheim (9th century), Saxon count and father of St Matilda * Dietrich Bonhoeffer (1906–1945), German Lutheran pastor and theologian * Wilhelm Dietrich von Buddenbrock (1672–1757), Prussian field marshal and cavalry leader * Dieterich Buxtehude (c. 1637/39–1707), Danish-German composer and organist * Dietrich von Choltitz (1894–1966), German General and last commander of Nazi-occupied Paris in 1944 * Dietrich Eckart (1868–1923), German politician * Dietrich Enns (born 1991), American baseball player * Dietrich Fischer-Dieskau (1925–2012), German baritone singer * Dietrich von Hildebrand (1889–1977), German Catholic philosopher and theologian * Dietrich Hollind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Downcutting
Downcutting, also called erosional downcutting, downward erosion or vertical erosion is a geological process by hydraulic action that deepens the channel of a stream or valley by removing material from the stream's bed or the valley's floor. The speed of downcutting depends on the stream's ''base level'', the lowest point to which the stream can erode. Sea level is the ultimate base level, but many streams have a higher "temporary" base level because they empty into another body of water that is above sea level or encounter bedrock that resists erosion. A concurrent process called lateral erosion refers to the widening of a stream channel or valley. When a stream is high above its base level, downcutting will take place faster than lateral erosion; but as the level of the stream approaches its base level, the rate of lateral erosion increases. This is why streams in mountainous areas tend to be narrow and swift, forming V-shaped valleys, while streams in lowland areas tend to be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Uplift
Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. Tectonic uplift results in denudation (processes that wear away the earth's surface) by raising buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies. Crustal thickening Crustal thickening has an upward component of motion and often occurs when continental crus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Veldenz
Veldenz is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Bernkastel-Wittlich district in Rhineland-Palatinate, Germany. It is the former main seat of the County of Veldenz, once a prominent principality to which belonged 120 villages and towns now in Rhineland-Palatinate and northern Alsace and Lorraine. Geography Location The municipality lies in the Middle Moselle region of valley country marked by even slopes and former oxbows of the Moselle. Veldenz is found on the Moselle's right bank, but does not lie right at the water's edge, but rather some two kilometres back from the river, under the outermost forests of the Hunsrück. Roughly 850 ha of the 1 441 ha municipal area is wooded. About 130 ha is given over to winegrowing. Veldenz belongs to the ''Verbandsgemeinde'' of Bernkastel-Kues, whose seat is in the like-named town. Nearby municipalities Neighbouring municipalities ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
