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Brandeckkopf
The Brandeckkopf is , and the highest mountain in the borough of Offenburg Offenburg ("open borough" - coat of arms showing open gates; Low Alemannic German, Low Alemmanic: ''Offäburg'') is a city located in the state of Baden-Württemberg, Germany. With nearly 60,000 inhabitants (2019), it is the largest city and the ad .... At 686.1 metres above sea level, the Brandeckkopf is the highest mountain of Offenburg. It is located within the Zell-Weierbach district. The ''Brandeckturm'', an observation tower, stands at the summit. The mountain is said to have been given its name by the Celts, who brought burnt offerings here. The mountain lies within the 1897 hectare ''Brandeck'' landscape protection area. References Mountains and hills of Baden-Württemberg Mountains and hills of the Black Forest Mountains under 1000 metres {{BadenWürttemberg-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Black Forest
The list contains a selection of the mountains and hills in the Black Forest, in order of their height.''Wandern im Schwarzwald'' . Over 1,400 m 
* Feldberg (1,493 m),August Vetter: ''Feldberg''. 2nd revised edition, 1996 highest mountain in the German
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Central Black Forest
The Central Black Forest (german: Mittlerer Schwarzwald), also called the Middle Black Forest, is a natural or cultural division of the Black Forest in Baden-Württemberg in Germany. It generally refers to a region of deeply incised valleys from the Rench valley and southern foothills of the Kniebis in the north to the area of Freiburg im Breisgau and Donaueschingen in the south. Its highest area, which is southeast of the Elz valley, is also part of the High Black Forest. Geography The dominating valley system of the Kinzig cuts through the Middle Black Forest from east to west. Prominent peaks are the Kandel (), Weißtannenhöhe (), Obereck (), Rohrhardsberg (), Brend (), Stöcklewald () and Mooswaldkopf () south of the Kinzig, and the Brandenkopf () and Lettstädter Höhe () north of the Kinzig. Geology Gneisses and granites predominate. Unlike the Northern Black Forest the Bunter sandstone covering with its plateau-like mountain shapes has only survived in a few pl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baden-Württemberg
Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a total area of nearly , it is the third-largest German state by both area (behind Bavaria and Lower Saxony) and population (behind North Rhine-Westphalia and Bavaria). As a federated state, Baden-Württemberg is a partly-sovereign parliamentary republic. The largest city in Baden-Württemberg is the state capital of Stuttgart, followed by Mannheim and Karlsruhe. Other major cities are Freiburg im Breisgau, Heidelberg, Heilbronn, Pforzheim, Reutlingen, Tübingen, and Ulm. What is now Baden-Württemberg was formerly the historical territories of Baden, Prussian Hohenzollern, and Württemberg. Baden-Württemberg became a state of West Germany in April 1952 by the merger of Württemberg-Baden, South Baden, and Württemberg-Hohenzollern. The ... [...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] |
Offenburg
Offenburg ("open borough" - coat of arms showing open gates; Low Alemannic German, Low Alemmanic: ''Offäburg'') is a city located in the state of Baden-Württemberg, Germany. With nearly 60,000 inhabitants (2019), it is the largest city and the administrative capital of the Ortenaukreis. History In recent times the remains of Roman settlements have been found within the city's territory. Offenburg was first mentioned in historical documents dating back to 1148. Offenburg had already been declared a Free Imperial City by 1240. In September 1689, the city - with the exception of two buildings - was totally destroyed by the French during the Nine Years War. Due to Napoleon's dissolution of the Holy Roman Empire in 1803 and subsequent reorganization of the German states, Offenburg lost its status as a Free Imperial City and fell under the rule of the Grand Duchy of Baden. During the outbreak of the Revolutions of 1848 in the German states#Baden, Revolutions of 1848, the "''Offenbur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Baden-Württemberg
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
