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Tertiary Hills
The Tertiary Hill Country (german: Tertiärhügelland or ''Tertiäres Hügelland''), also called the Tertiary Hills, is an upland area with a moderate climate in the northern Alpine Foreland, which extends northwards as far as the River Danube. It is divided into two simple contiguous regions that are separated by the valley of the Lower Inn which itself is not usually counted as part of the Tertiary Hills. In Germany (Bavaria), the Lower Bavarian Upland is its larger northwestern element; in Upper Austria it forms the Hausruckviertl Mountain and Hill Country (also called the Upper Austrian Hill Country or ''Oberösterreichisches Hügelland''). From a natural regional perspective, depending on the definition, it forms one or two 3rd level natural regions. The Tertiary Hill Country is bordered to the west, south and southeast by old moraine gravel plateaux, that also form 3rd order major regions in the northern Alpine Foreland: * the Iller-Lech Plateau The Iller-Lech Plateau (g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Foreland
The Alpine Foreland, less commonly called the Bavarian Foreland,Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, pp. 585-586. . Bavarian Plateau or Bavarian Alpine Foreland (german: Bayerisches Alpenvorland), refers to a triangular region of plateau and rolling foothills in Southern Germany, stretching from Lake Constance in the west to beyond Linz on the Danube in the east, with the Bavarian Alps forming its south boundary and the Danube its northern extent. Geography The Alpine Foreland has been shaped under the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quaternary sediments —silt and clay, sand and sedimentary rocks from Alpine erosion— overlay the Alpine nappes. Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region. The Alpine Foreland is crossed by the rivers Iller, Wertach, Lech, Isar a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Danube
The Danube ( ; ) is a river that was once a long-standing frontier of the Roman Empire and today connects 10 European countries, running through their territories or being a border. Originating in Germany, the Danube flows southeast for , passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine before draining into the Black Sea. Its drainage basin extends into nine more countries. The largest cities on the river are Vienna, Budapest, Belgrade and Bratislava, all of which are the capitals of their respective countries; the Danube passes through four capital cities, more than any other river in the world. Five more capital cities lie in the Danube's basin: Bucharest, Sofia, Zagreb, Ljubljana and Sarajevo. The fourth-largest city in its basin is Munich, the capital of Bavaria, standing on the Isar River. The Danube is the second-longest river in Europe, after the Volga in Russia. It flows through much of Central and Sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Inn
{{Disambiguation ...
Lower may refer to: *Lower (surname) *Lower Township, New Jersey *Lower Receiver (firearms) *Lower Wick Gloucestershire, England See also *Nizhny Nizhny (russian: Ни́жний; masculine), Nizhnyaya (; feminine), or Nizhneye (russian: Ни́жнее; neuter), literally meaning "lower", is the name of several Russian localities. It may refer to: * Nizhny Novgorod, a Russian city colloquial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Bavarian Upland
The Lower Bavarian Upland, Lower Bavarian Hill Country (German: ''Niederbayerisches Hügelland'') or Lower Bavarian Hills, are part of the tertiary '' Hügelland'' or hill country south of the River Danube and cover much of the land within the Bavarian province of Lower Bavaria in southern Germany. To the north it is bordered by the Gäuboden region and the Bavarian Forest; to the south by Upper Bavaria, to the east by the Lower Inn Valley and to the west by the Franconian Jura (''Fränkische Alb''). In the western part of the Lower Bavarian Hills lies the Hallertau, the world's largest hop-growing region.Bentley, James; Catling, Christopher; & Locke, Tim (1994). ''Munich and Bavaria''. Chicago: Passport Books. It belongs to two of officially defined natural regions in Germany: the eponymous Lower Bavarian hills and the Isar-Inn Gravel Beds (''Isar-Inn-Schotterplatten'') and is sub-divided into the Danube-Isar Hills (''Donau-Isar-Hügelland'') and the Isar-Inn Upland (''Isa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Austria
Upper Austria (german: Oberösterreich ; bar, Obaöstareich) is one of the nine states or of Austria. Its capital is Linz. Upper Austria borders Germany and the Czech Republic, as well as the other Austrian states of Lower Austria, Styria, and Salzburg. With an area of and 1.49 million inhabitants, Upper Austria is the fourth-largest Austrian state by land area and the third-largest by population. History Origins For a long period of the Middle Ages, much of what would become Upper Austria constituted Traungau, a region of the Duchy of Bavaria. In the mid-13th century, it became known as the Principality above the Enns River ('), this name being first recorded in 1264. (At the time, the term "Upper Austria" also included Tyrol and various scattered Habsburg possessions in South Germany.) Early modern era In 1490, the area was given a measure of independence within the Holy Roman Empire, with the status of a principality. By 1550, there was a Protestant majority. In 1564, ... [...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] |
Natural Regions Of Germany
This division of Germany into major natural regions takes account primarily of geomorphological, geological, hydrological, and pedological criteria in order to divide the country into large, physical units with a common geographical basis. Political boundaries play no part in this, apart from defining the national border. In addition to a division of Germany by ''natural regions'', the federal authorities have also produced a division by so-called ''landscape areas (Landschaftsräume)'' that is based more on human utilisation of various regions and so has clearly different boundaries. Groundwork by the Federal Institute of Regional Studies (BfL) The natural region classification of Germany, as used today by the Federal Office for Nature Conservation (''Bundesamt für Naturschutz'' or BfN) and by most state institutions, is largely based on the work in producing the Handbook of Natural Region Divisions of Germany between the years 1953 to 1962. This divided the present federal t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Moraine
Old and Young Drift are geographic names given to the morainic landscapes that were formed in Central Europe; the Old Drift during the older ice ages and the Young Drift during the latest glaciations – the Weichselian in North Germany and the Würm in the Alps. Their landforms are quite different. Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes such as denudation and erosion, whilst areas of Young Drift have largely retained their original shape. Whilst the majority of Old Drift moraines were formed during the Saale glaciation about 130,000 to 140,000 years ago, the Young Drift moraines in Central Europe are only about 15,000 to 20,000 years old. The terms Old and Young Drift are used for all elements of the glacial series even though the meltwater deposits and landforms are not strictly moraines. Old Drift The Old Drift landscapes were tundras or cold deserts during the last ice age. Periglacial processes resulted in signi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
