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Leipzig Bay
The Leipzig BayDickinson (1964), p. 29.''Utrata Fachwörterbuch: Geographie - Englisch-Deutsch/Deutsch-Englisch'' by Jürgen Utrata (2014). Retrieved 10 Apr 2014.(german: Leipziger Tieflandsbucht) or Leipzig Basin or Saxon LowlandDickinson (1964), p. 37. or Saxon Bay is a relatively lakeless and highly fertile in |
Merseburg
Merseburg () is a town in central Germany in southern Saxony-Anhalt, situated on the river Saale, and approximately 14 km south of Halle (Saale) and 30 km west of Leipzig. It is the capital of the Saalekreis district. It had a diocese founded by Archbishop Adalbert of Magdeburg. The University of Merseburg is located within the town. Merseburg has around 33,000 inhabitants. Names * cs, Merseburk, Meziboř * french: Mersebourg * german: Merseburg * la, Merseburga * pl, Międzybórz * wen, Mjezybor Geography The town Merseburg consists of Merseburg proper and the following four ''Ortschaften'' or municipal divisions:Hauptsatzung der Stadt Merseburg § 15, April 2019. * |
Structural Basin
A structural basin is a large-scale structural formation of rock strata formed by tectonic warping of previously flat-lying strata. They are geological depressions, the inverse of domes. Elongated structural basins are also known as synclines. Some are sedimentary basins, aggregations of sediment that filled up a depression or accumulated in an area. Others were formed by tectonic events long after the sedimentary layers were deposited. Basins may appear on a geologic map as roughly circular or elliptical, with concentric layers. Because the strata dip toward the center, the exposed strata in a basin are progressively younger from the outside in, with the youngest rocks in the center. Basins are often large in areal extent, often hundreds of kilometers across. Structural basins are often important sources of coal, petroleum, and groundwater. Examples Europe * Hampshire Basin, United Kingdom * London Basin, United Kingdom * Paris Basin, France * Permian Basin, Poland, northern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vogtland
Vogtland (; cz, Fojtsko) is a region spanning the German states of Bavaria, Saxony and Thuringia and north-western Bohemia in the Czech Republic. It overlaps with and is largely contained within Euregio Egrensis. The name alludes to the former leadership by the Vögte ("advocates" or "lords protector") of Weida, Gera and Plauen. Geography Natural geography The landscape of the Vogtland is sometimes referred to as idyllic, bearing in mind its fields, meadows and wooded hilltops. In the south and southeast, Vogtland rises to a low or mid-height mountain range also called ''Oberes Vogtland'', or Upper Vogtland. Here, monocultural coniferous forest is the predominant form of vegetation. The Vogtland's highest mountain is Schneehübel, reaching 974 metres; another remarkable landmark is the Schneckenstein, 883 m above sea level, which gained some renown for its (falsely) alleged unique abundance of topaz crystals. Its mountains spread from Ore Mountains in the so ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleiße
The Pleiße is a river of Saxony and Thuringia, Germany. The Pleiße has its source southwest of Zwickau at Ebersbrunn, then flows through Werdau, Crimmitschau, Altenburg, and other towns and villages in Saxony and Thuringia, before flowing from the right into the White Elster in Leipzig. The river originally had a natural length of ; however, south of Leipzig, it has been straightened, which shortened it to around . See also * Kleine Pleiße * List of rivers of Saxony * List of rivers of Thuringia A list of rivers of Thuringia, Germany: A *Alster * Apfelstädt * Ascherbach * Auma B * Biber * Bibra * Blambach * Bode * Breitenbach *Breitstrom D *Dammbach * Deube * Dober * Dürrbach E * Effelder * Eichbach * Ellenbach *Eller *Elschni ... Notes *The information in this article is based on and/or translated from its German equivalent. External links * Rivers of Saxony Rivers of Thuringia Rivers of Germany {{Thuringia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mulde
The Mulde () is a river in Saxony and Saxony-Anhalt, Germany. It is a left tributary of the Elbe and is long. The river is formed by the confluence, near Colditz, of the Zwickauer Mulde (running through Zwickau) and the Freiberger Mulde (with Freiberg on its banks), both rising from the Ore Mountains. From here the river runs northwards through Saxony (Grimma, Wurzen, Eilenburg, Bad Düben) and Saxony-Anhalt (Jeßnitz and Dessau, the old capital of Anhalt). The Mulde flows into the Elbe north of Dessau.1911 Encyclopædia Britannica In August 2002 a flood caused severe damage, that even endangered the UNESCO World Heritage Site "Dessau-Wörlitzer Gartenreich" and the city Dessau. Its name could be derived from Old German (possibly Gothic) "Mulda" (𐌼ᚢ𐌻ᛞᚨ), meaning "dust" and a cognate of English " mould"). But more possibly it is related to the German "mahlen" which means "to mill". Therefore, Mulde probably means "the milling river" and corresponds to the great ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Elster
The White Elster Accessed on 16 Jan 2011. (, ) is a long river in central , right tributary of the . Its source is in the westernmost part of the , in the territory of . After a few kilometres, it flows into eastern where it cuts through the |
Saale
The Saale (), also known as the Saxon Saale (german: Sächsische Saale) and Thuringian Saale (german: Thüringische Saale), is a river in Germany and a left-bank tributary of the Elbe. It is not to be confused with the smaller Fränkische Saale, Franconian Saale, a right-bank tributary of the Main (river), Main, or the Saale (Leine), Saale in Lower Saxony, a tributary of the Leine. Etymology The name ''Saale'' comes from the Proto-Indo-European language, Proto-Indo-European root wikt:Reconstruction:Proto-Indo-European/sélos, *''séles'' 'marsh', akin to Welsh language, Welsh ''hêl, heledd'' 'river meadow', Cornish language, Cornish ''heyl'' 'estuary', Ancient Greek, Greek ''hélos'' 'marsh, meadow', Sanskrit ''sáras'' 'lake, pond', Sarasvati River, ''Sárasvati'' 'sacred river', Old Persian ''Harauvati'' 'Harut River, Hārūt River; Arachosia', Avestan ''Haraxvatī'', idem. It may also be related to the Indo-European root *''sal'', "salt". The Slavic name of the Saale, ''Sola ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohburg Hills
The Hohburg Hills (german: Hohburger Berge), also called Hohburg Switzerland (''Hohburger Schweiz''), are located in the district of Nordsachsen near the eponymous village of Hohburg in the municipality of Lossatal in the German state of Saxony. Geography These quartz-porphyry hills rise prominently up to 120 metres out of the surround plain of the Leipzig Bay, east of the River Mulde. Their highest point is the Löbenberg at (). Other high points are the Gaudlitzberg (), the Burzelberg () and the Galgenberg ("Gallows Hill", ). South of Hohburg is the Kleine Berg ("Little Hill") with a height of . In the valley lying amongst the Hohburg Hills, the stream of the Lossabach flows through Müglenz, Hohburg, Klein- and Großzschepa to empty into the Mulde near Thallwitz. History The Hohburg Hills were shaped by decades of intensive stone quarrying. This produced steep rock faces and several lakes in the hollows that were left behind. The rock faces, up to forty meters high, ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plain
In geography, a plain is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or uplands. In a valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs. Where a geological region contains more than one plain, they may be connected by a pass (sometimes termed a gap). Coastal plains mostly rise from sea level until they run into elevated features such as mountains or plateaus. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. Plains can be formed from flowing lava; from deposition of sediment by water, ice, or wind; or formed by erosion by the agents from hills and mountains. Biomes on plains include grassland ( temperate or subtr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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