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Acher Rench Correction
The Acher is a 53.6-kilometre-long river and right-hand tributary of the Rhine in the county of Ortenau, in the south German state of Baden-Württemberg. It flows in an northwesterly direction from the Black Forest to the Rhine, between the two rivers Rench to the south and the Oos to the north. Geography The source region of the Acher lies on the northeastern mountainside of the Vogelskopf () an area divided into cirques formed by the ice age. The spring named the ''Acherquelle'' rises at a height of in the area of the ''Ruhesteinloch'', which is named after the Ruhestein Saddle to the east and is located between the Vogelskopf and Seekopf (). The Acher initially flows northwards, descending steeply. At its confluence with the Seebach, which joins from the north from the Mummelsee below the Hornisgrinde, it turns westwards and flows through the trough-like valley of Seebach. Here the valley reaches a depth of about 550 metres between the Hornisgrinde and the Vogelskopf. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trough Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foothill Zone (Upper Rhine Graben)
The foothill zone of the Upper Rhine Plain (german: Vorbergzone des Oberrheingraben) is the hill country in front of the mountains either side of the Upper Rhine Plain, especially those in front of the Black Forest, Vosges and Palatinate Forest. When the rift valley sank the foothills on the flanks of the mountain ranges were left hanging as fault blocks. The strata of the platform have been preserved in this zone, whereas they have been eroded from the neighbouring higher blocks. They are usually covered by a layer of loess and offer good conditions for agricultural use. For example, in Baden, the Alsace Alsace (, ; ; Low Alemannic German/ gsw-FR, Elsàss ; german: Elsass ; la, Alsatia) is a cultural region and a territorial collectivity in eastern France, on the west bank of the upper Rhine next to Germany and Switzerland. In 2020, it had ... and the Palatinate intensive orchard and vineyard cultivation is practised in the foothill zone. External links * (pdf; 1.8&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Achern
Achern (; gsw, label= Low Alemannic, Achre) is a town in Western Baden-Württemberg, Germany. It is located approximately 18 km southwest of Baden-Baden and 19 km northeast of Offenburg. Achern is the fourth largest town in the district of Ortenau (Ortenaukreis), after Offenburg, Lahr / Black Forest and Kehl. As subsequent to the district reform in the 1970s the population passed the 20,000 mark, Achern requested to be awarded the status of ''Große Kreisstadt''. The status was granted by the State government effective January 1, 1974. Achern collaborates with the communities of Lauf, Sasbach, and Sasbachwalden in administrative matters. Besides Achern itself, the municipality includes the boroughs of Fautenbach, Gamshurst, Großweier, Mösbach, Oberachern, Önsbach, Sasbachried and Wagshurst. Geography Geographic location Achern is located in the northern Black Forest near the Hornisgrinde, at the entrance to the Acher Valley and not far from the eastern edge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa colli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kappelrodeck
Kappelrodeck ( gsw, label= Low Alemannic, Kabbl) is a town in Western Baden-Württemberg, Germany and belongs to the district of Ortenau. It is located at the western hillslope of the Black Forest in the valley Achertal. It is about 20 kilometres to the north of Offenburg and about 20 kilometres to the south of Baden-Baden. In clear weather, the city of Strasbourg in France can be seen which is roughly 25 kilometres to the west of Kappelrodeck. History Kappelrodeck was mentioned as ''A Capelle apud Rodecke'' in a document dated 1349. The town part ''Waldulm'' was documented a 100 years prior in 1244. The name relates to a chapel that was located below the castle ''Rodeck''. Initially, Kappelrodeck was part of the land controlled by the prince-bishop of Strasbourg. During the Thirty Years' War and the French revolution, Kappelrodeck suffered from cruelties by every side. In 1803, Kappelrodeck was transferred to the house of Baden A house is a single-unit residential buildin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ottenhöfen Im Schwarzwald
Ottenhöfen im Schwarzwald ( gsw, label= Low Alemannic, Oddeheefe) is a town in the district of Ortenau in Baden-Württemberg in Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... References Ortenaukreis {{Ortenaukreis-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
