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Hotzenwald
The Hotzenwald is a landscape and region in the Southern Black Forest in the county of Waldshut. Its headquarters was the ''Waldvogteiamt''. Location and topography The region of Hotzenwald is not precisely defined in the records. In a narrower sense the Hotzenwald is the southernmost region of the Southern Black Forest, bounded in the west roughly by the Wehra, in the north approximately by the upper reaches of the Alb River near St. Blasien, in the east by the hill ridge between the Alb and Schlücht rivers, and in the south by the High Rhine and Klettgau rivers. This definition of the Hotzenwald more or less covers the same area as the territory of the former County of Hauenstein. In a wider sense, other regions may be counted as part of the Hotzenwald that were linked to St. Blaise Abbey or the County of Hauenstein, both of which were historically important in the Southern Black Forest. These additional areas include, for example, the parish of Gersbach (Schopfheim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hotzenwald Region
The Hotzenwald is a landscape and region in the Southern Black Forest in the county of Landkreis Waldshut, Waldshut. Its headquarters was the ''Waldvogteiamt''. Location and topography The region of Hotzenwald is not precisely defined in the records. In a narrower sense the Hotzenwald is the southernmost region of the Southern Black Forest, bounded in the west roughly by the Wehra, in the north approximately by the upper reaches of the Alb River (High Rhine), Alb River near St. Blasien, in the east by the hill ridge between the Alb and Schlücht rivers, and in the south by the High Rhine and Klettgau rivers. This definition of the Hotzenwald more or less covers the same area as the territory of the former County of Hauenstein. In a wider sense, other regions may be counted as part of the Hotzenwald that were linked to St. Blaise Abbey, Black Forest, St. Blaise Abbey or the County of Hauenstein, both of which were historically important in the Southern Black Forest. These addit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wehra
Wehra is a river of Baden-Württemberg, Germany. It passes through Todtmoos and Wehr and flows into the Rhine downstream of Bad Säckingen. Geography Location and topography The valley of the Wehra is distinctly divided into three sections. The upper reaches are a high valley typical of the Black Forest, but at 200 to 300 meters deep, they are significantly more relief-like than the neighboring high valleys of the Hotzenwald to the east. Its center is the village of Todtmoos, which occupies the largest part of the valley, which was noticeably reshaped by ice-age glaciers. In its middle course, the Wehra cuts a gorge, sometimes over 400 meters deep, into the southwestern slopes of the Black Forest. Steep, wooded slopes alternate with cliffs almost 100 meters high in some places. This steep section of the river is a nationally renowned, extremely difficult whitewater stretch. A rocky outcrop there bears the name ''Hirschsprung (''Stag's Leap). The approximately seven-kilomet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Görwihl
Görwihl is a municipality in the district of Waldshut in Baden-Württemberg in Germany. History The name is derived from the ancient German for spear, due to the spearhead shape of the area at the time. Görwihl was established in 1193, and was first recorded as ''Gerswillare''. Like many places in the region, Görwihl belonged to the county Hauenstein within Further Austria. It became the centre of legal activity for the region and played a role in the peasants' uprising. In 1806, Görwihl became part of the newly created Grand Duchy of Baden. The community in its present scale was developed in the context of Baden-Wurttemberg regional reform. Rotzingen joined the municipality of Görwihl in 1971 and Hartschwand in 1972, with the other districts following in 1975. Geography Görwihl is within the Hotzenwald region, and lies in the southernmost part of the Black Forest, at the edge of the River Alb, a tributary of the Rhine. The landscape of the region is characterized by h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bad Säckingen
Bad Säckingen (; High Alemannic: ''Bad Säckinge'') is a rural town in the administrative district of Waldshut in the state of Baden-Württemberg in Germany. It is famous as the "Trumpeter's City" because of the book ''Der Trompeter von Säckingen'' ("The Trumpeter of Säckingen"), a famous 19th-century novel by German author Joseph Victor von Scheffel. Geography Bad Säckingen is located in the very southwest of Germany on the High Rhine next to the Swiss border. The city lies on the southern edge of the Hotzenwald, which is the southern foothills of the Black Forest. Constitutuent communities The town of Bad Säckingen consts of the following former municipalities: * Harpolingen with the farms Lochmühle and Rüttehof and the houses Holdmatt * Rippolingen with the Flut farmstead and the Santihof houses * Säckingen with the district of Obersäckingen and the houses Am Bergsee * Wallbach Nearby places *Close (15 km): Waldshut-Tiengen, Schopfheim, Lörrach, Basel, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Rhine
High Rhine (, ; kilometres 0 to 167 of the Rhine) is the section of the Rhine between Lake Constance () and the city of Basel, flowing in a general east-to-west direction and forming mostly the Germany–Switzerland border. It is the first of four named sections of the Rhine (High Rhine, Upper Rhine, Middle Rhine, Lower Rhine) between Lake Constance and the Rhine–Meuse–Scheldt delta, river delta at the North Sea. Name The term ''High Rhine'' was introduced by scientists in the 19th century. Above all geologists tried to differentiate the High Rhine () linguistically from the Upper Rhine (, ). Until the 19th century, it was also known as the 'Badisch-Swiss Rhine'. It lends its name to the High Rhine Railway line, which to a great extend follows the river to the north of it. Geography Course The High Rhine begins at the outflow of the Rhine from the ''Untersee (Lake Constance), Untersee'' (Lower Lake Constance) in Stein am Rhein and turns into the Upper Rhine at the Rhine knee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dachsberg (Southern Black Forest)
Dachsberg is a municipality in the district of Waldshut in Baden-Württemberg in Germany Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu .... References Waldshut (district) Hotzenwald {{Waldshut-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Greek ''palaiós'' (παλαιός, "old") and ''zōḗ'' (ζωή, "life") meaning "ancient l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Migmatite
Migmatite is a composite rock (geology), rock found in medium and high-grade metamorphic environments, commonly within Precambrian craton, cratonic blocks. It consists of two or more constituents often layered repetitively: one layer is an older metamorphic rock that was reconstituted subsequently by partial melting ("paleosome"), while the alternate layer has a Pegmatite, pegmatitic, Aplite, aplitic, Granite, granitic or generally plutonic appearance ("neosome"). Commonly, migmatites occur below deformed metamorphic rocks that represent the base of eroded mountain chains. Migmatites form under extreme temperature and pressure conditions during Metamorphism#Prograde and retrograde, prograde metamorphism, when partial melting occurs in metamorphic paleosome. Components Solid solution, exsolved by partial melting are called neosome (meaning ‘new body’), which may or may not be heterogeneous at the microscopic to macroscopic scale. Migmatites often appear as tightly, incoheren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss (pronounced ) 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. This rock is formed under pressures ranging from 2 to 15 kbar, sometimes even more, and temperatures over 300 °C (572 °F). Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct Cleavage (geology), cleavage. Gneisses are common in the ancient crust of Continental Shield, continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description image:Orthogneiss Geopark.jpg, 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 (geology), cleavage. In other words, it i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, 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 dike (geology), 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 diagram, 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) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steina (Wutach)
Steina is a river of Baden-Württemberg, Germany. It flows into the Wutach near Lauchringen. See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A *Aal (Kocher), Aal *Aalbach (Main), Aalbach *Aalenbach *Ablach (Danube), Ablach *Ach (Blau), Ach *Acher *Adelbach *Aich (river), Aich *Aid (Würm), Aid *Aischbach (Kinzig), Aischbach, tributary ... References Rivers of Baden-Württemberg Rivers of the Black Forest Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
