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Belchen (Black Forest)
The Belchen, , or Black Forest Belchen (german: Schwarzwälder Belchen) is the fourth-highest summit of the Black Forest after Feldberg, Seebuck and Herzogenhorn. The municipalities of Münstertal, Schönenberg and Kleines Wiesental meet on the summit dome of Belchen which is located in the southwest German state of Baden-Württemberg. Geography The Belchen, with its furrowed, unbroken rock faces, rises 1,000 metres out of the Münstertal valley. Its north face is thus the area of highest relief energy in the German Central Uplands. Even towards the south the mountain drops steeply, its ''schrofen'' slopes descending 800 metres into the valley bowl of the Little Wiese near Neuenweg. The large expanse of rolling plateau in the eastern Black Forest has only survived in small places at the Belchen. Towards the Rhine Plain and the Blauen mountain the western main crest of the southern Black Forest has been cut into narrow ridges as a result of the marked uplift of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blauen (Badenweiler)
Blauen or Hochblauen is a mountain in the southern Black Forest. The peak lies within the municipalities of Schliengen and Malsburg-Marzell in Landkreis Lörrach and the community of Badenweiler in Breisgau-Hochschwarzwald. It is an ideal viewpoint with views of the Black Forest, Vosges, Jura Mountains, and the Alps. Name In the 14th century, the mountain was recorded as the ''Blauwen'' or ''Blawen''. Matthäus Merian's '' Topographia Sueviae'' in the mid-17th century calls it the ''Hoche Blawen'' ("High Blawen"). The parish boundary plan of the first Baden state survey of 1769/1770 distinguishes between the ''Hoch Blauen'' ("High Blauen") and the ''Hinter Blauen'' ("Posterior Blauen"), a sub-peak, north-northeast of the main summit. As the ''Blauen M ns' the mountain is shown on the Black Forest map owned by St. Blaise Abbey dating to the year 1788. And in 1845 in the ''Topographischen Atlas ueber das Grossherzogtum Baden'' ("Topographic Atlas of the Grand Duchy of Baden") ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vosges
The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort–Ronchamp– Lure line) to the Börrstadt Basin (the Winnweiler– Börrstadt–Göllheim line), and forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at , followed by the Storkenkopf (), and the Hohneck ().IGN maps available oGéoportail/ref> Geography Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alsatian Belchen
The Ballon d'Alsace german: Elsässer Belchen (el. 1247 m.), sometimes also called the Alsatian Belchen to distinguish it from other mountains named "Belchen" is a mountain at the border of Alsace, Lorraine, and Franche-Comté. From its top, views include the Vosges, the Rhine valley, the Black Forest, and the Alps. A road leads over a pass near the peak at the Col du Ballon d'Alsace, . The pass is noted as the site of the first official mountain climb in the Tour de France on 11 July 1905, the first rider to the top of the climb being René Pottier and the stage being won by Hippolyte Aucouturier. Stage 9 of the 2005 Tour crossed this pass on the centenary of the original climb. Ballon d'Alsace features Alpine and Cross Country skiing tracks. The mountain is part of the so-called Belchen System, a group of mountains with the name "Belchen" (in German) that may have been part of a Celtic sun calendar. Geography Climate Ballon d'Alsace has a humid continental climate (Köppen c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belchen Triangle
The Belchen System refers to five mountains with the name ''Belchen'' around the tripoint of Germany, France and Switzerland that may have been used by the Celts as a solar calendar. The term is an extension of the Belchen Triangle. The mountains are: * ''Belchen'', or Black Forest Belchen * ''Belchenflue'', or Swiss Belchen * ''Ballon d'Alsace'', or Alsatian Belchen * ''Grand Ballon'', or Great Belchen * ''Petit Ballon'', or Little Belchen Geographical description The heart of the Belchen System is the southernmost mountain of the Vosges, the ''Ballon d'Alsace'' (''Elsässer Belchen'' or Alsatian Belchen, 1,247 metres). Seventy three kilometres due east is the Black Forest Belchen (''Schwarzwälder Belchen'', 1,414 metres), which is only 167 metres higher and over which the sun rises at the equinoxes, i.e. at the beginning of spring and autumn, as seen from Grand Ballon. Conversely, the sun sets over the Alsatian Belchen on these days when seen from the Black For ... [...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] |
Margraviate Of Baden
The Margraviate of Baden (german: Markgrafschaft Baden) was a historical territory of the Holy Roman Empire. Spread along the east side of the Upper Rhine River in southwestern Germany, it was named a margraviate in 1112 and existed until 1535, when it was split into the two margraviates of Baden-Durlach and Baden-Baden. The two parts were reunited in 1771 under Margrave Charles Frederick, even if the three parts of the State maintained their distinct seats to the Reichstag.Votes number 58 Baden, 60 Durlach, 62 Höchberg. The restored Margraviate of Baden was elevated to the status of electorate in 1803. In 1806, the Electorate of Baden, receiving territorial additions, became the Grand Duchy of Baden. The rulers of Baden, known as the House of Baden, were a cadet line of the Swabian House of Zähringen. History During the 11th century, the Duchy of Swabia lacked a powerful central authority and was under the control of various comital dynasties, the strongest of them being ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Further Austria
Further Austria, Outer Austria or Anterior Austria (german: Vorderösterreich, formerly ''die Vorlande'' (pl.)) was the collective name for the early (and later) possessions of the House of Habsburg in the former Swabian stem duchy of south-western Germany, including territories in the Alsace region west of the Rhine and in Vorarlberg. While the territories of Further Austria west of the Rhine and south of Lake Constance (except Konstanz itself) were gradually lost to France and the Swiss Confederacy, those in Swabia and Vorarlberg remained under Habsburg control until the Napoleonic Era. Geography Further Austria mainly comprised the Alsatian County of Ferrette in the Sundgau, including the town of Belfort, and the adjacent Breisgau region east of the Rhine, including Freiburg im Breisgau after 1368. Also ruled from the Habsburg residence in Ensisheim near Mühlhausen were numerous scattered territories stretching from Upper Swabia to the Allgäu region in the east, the large ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Habsburg
The House of Habsburg (), alternatively spelled Hapsburg in Englishgerman: Haus Habsburg, ; es, Casa de Habsburgo; hu, Habsburg család, it, Casa di Asburgo, nl, Huis van Habsburg, pl, dom Habsburgów, pt, Casa de Habsburgo, la, Domus Habsburg, french: Maison des Habsbourg and also known as the House of Austriagerman: link=no, Haus Österreich, ; es, link=no, Casa de Austria; nl, Huis van Oostenrijk, pl, dom Austrii, la, Domus Austriæ, french: Maison d'Autriche; hu, Ausztria Háza; it, Casa d'Austria; pt, Casa da Áustria is one of the most prominent and important dynasties in European history. The house takes its name from Habsburg Castle, a fortress built in the 1020s in present-day Switzerland by Radbot of Klettgau, who named his fortress Habsburg. His grandson Otto II, Count of Habsburg, Otto II was the first to take the fortress name as his own, adding "Count of Habsburg" to his title. In 1273, Count Radbot's seventh-generation descendant Rudolph I of German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boundary Stone
A boundary marker, border marker, boundary stone, or border stone is a robust physical marker that identifies the start of a land boundary or the change in a boundary, especially a change in direction of a boundary. There are several other types of named border markers, known as boundary trees, pillars, monuments, obelisks, and corners. Border markers can also be markers through which a border line runs in a straight line to determine that border. They can also be the markers from which a border marker has been fixed. Purpose According to Josiah Ober, boundary markers are "a way of imposing human, cultural, social meanings upon a once-undifferentiated natural environment." Boundary markers are linked to social hierarchies, since they derive their meaning from the authority of a person or group to declare the limits of a given space of land for political, social or religious reasons. Ober notes that "determining who can use parcels of arable land and for what purpose, has imme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
