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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] |
Stöcklewald
The Stöcklewald is a mountain, , in the southern part of the Central Black Forest in Germany between the towns of Furtwangen and Triberg, each about 5 kilometres distant, in the county of Schwarzwald-Baar-Kreis. Towards the north, the Black Forest only exceeds this height again in the area of the Schliffkopf and the Hornisgrinde. Location The European Watershed between the Rhine and the Danube runs over the mountain. On its northern slopes rises the Gutach, which flows from here in a northwesterly direction through the Schönwald Highlands and drops over its northeastern edge as the Triberg Waterfalls. To the southeast flow the tributary streams of the Breg. The northern foot of its gently-sloping domed summit may be reached on local ''Landesstraßen'' and ''Kreisstraße''n, both from the aforementioned towns as well as from Schönwald and Brigach. From there a road runs up to the summit, where there is a ''Gasthaus'', a hiker's home belonging to the Black Forest Club and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schiltach (river)
The Schiltach (in its upper course also: ''Berneck'') is a river of Baden-Württemberg, Germany. It is a tributary of the Kinzig in the town Schiltach. See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach *Aalenbach * Ablach * Ach *Acher *Adelbach *Aich *Aid * Aischbach, tributary of the Kinzig * Aischbach, tributary of the Körsch * Aitrach, tributary of the Danube * Aitrach, tri ... References Rivers of Baden-Württemberg Rivers of the Black Forest Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Die Schwarzwaldklinik
''The Black Forest Clinic'' (german: Die Schwarzwaldklinik, ) is a German medical drama television series that was produced by and filmed in West Germany. The series was produced between 1984 and 1988 with the original airing being from October 2, 1985 to March 25, 1989 on West Germany's ZDF (Zweites Deutsches Fernsehen) television channel. The series' storyline follows the inner workings of a small fictional hospital in the Black Forest region of Germany as well as the lives of the Brinkmann family of doctors who work at the hospital. Shortly after broadcasting had begun in 1985, ''The Black Forest Clinic'' became a highly popular television event, reaching audiences of over 20 million viewers. 25 years since its debut, it is still highly regarded in Germany. The series had been re-broadcast several times since 1985 and has spawned two television films released 20 years after its initial airing. Background and development The creation of ''The Black Forest Clinic'' was influen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glottertal
Glottertal is a municipality in the district of Breisgau-Hochschwarzwald in Baden-Württemberg in southern Germany. History From 1567 till the Napoleonic Wars the area was part of Further Austria and therefore part of the Habsburg monarchy. Although the history of mining in the Glottertal goes back to Roman times and villages in the area are mentioned 1112 in the chronics of Abbey of Saint Peter in the Black Forest the municipal Glottertal was formed in 1970. The four former independent villages Unterglottertal, Oberglottertal, Ohrensbach und Föhrental were associated to the Glottertal municipal. Points of interest Buildings The 1914 built Carlsbau in Glottertal was the set for the 1980s medical drama television series ''The Black Forest Clinic''. The outside of the building and the surrounding area was filmed while the interior was filmed in a set in Hamburg. The building was used as a clinic till it was closed down in 2004.Luck, HarryDas Geisterhaus im Glottertal ''Focus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wilde Gutach
The Wild Gutach (german: Wilde Gutach) is a river in Baden-Württemberg, Germany. It flows into the Elz in Gutach im Breisgau. Sights and structures * Hexenlochmühle with two overshot water wheels in a ravine-like witch's hole (''Hexenloch'') * '' Balzer Herrgott'', a stone statue of Christ which has almost grown into a tree * '' Teichschlucht'' ravine below Gütenbach * '' Hirschbach Falls'' and '' Zweribach Waterfalls'' in the rugged Zweribach Cirque (''Bannwald'' and nature reserve) * ''Plattensee'' Reservoir in the high valley of the ''Platte'' of the Zweribach * '' Zweribachwerk'', power station above Simonswald * ''Brend'' summit * ''Kandel'' summit * '' Schultiskopf'' and ''Spitzer Stein'' (rocky arêtes) * '' Kostgfällschlucht'' with waterfalls and the ''Gfällfelsen'' rock formation (climbing area, nature reserve) * Chapel on the ''Hörnleberg'' See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach *Aa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Black Forest
The Southern Black Forest (german: Südschwarzwald) is the highest part of the Black Forest, an area heavily transformed by ice age glaciation south of a line roughly from Freiburg im Breisgau to Donaueschingen. The term High Black Forest is not quite identical; that usually includes the highest part of the Central Black Forest, southeast of the Elz valley, as well. The Southern Black Forest Nature Park (''Naturpark Südschwarzwald'') also takes in this area, extending across the whole of the High Black Forest as well as several peripheral areas. Characteristics Unlike the almost parallel mountain ridges and plateaux of the Northern Black Forest and the deeply incised central region, the Southern Black Forest is dominated by a central area of highland, from which most of the large valley emanate. The highest summits of the central highlands are the Feldberg () and the Herzogenhorn (). Towering prominently over the Rhine Plain are the Belchen (), the Schauinsland () and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Black Forest
The Northern Black Forest (german: Nordschwarzwald) refers to the northern third of the Black Forest in Germany or, less commonly today, to the northern half of this mountain region. Geography The Northern Black Forest is bounded in the north by a line from Karlsruhe to Pforzheim and, in the south, by a line running from the Rench valley to Freudenstadt. Its northern boundary largely coincides with the emergence of the extensively forested bunter sandstone strata from the arable region of the Kraichgau; its southern boundary with the Central Black Forest (or, in the case of a bipartite division, the Southern Black Forest) varies depending on the definition or natural regional division used (see also Black Forest). Earlier, the Northern Black Forest was the entire northern half of the mountain range as far as the Kinzig (Rhine), line of the Kinzig valley, which divides the Black Forest east of Lahr/Schwarzwald, Lahr. To the west it is bounded by the Upper Rhine Plain, to the east ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...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] |
