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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 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] |
Görwihl
Görwihl is a town 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 high plate ... [...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 "Trumpeteer'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 next to the Swiss border on the river Rhine. The city lies on the southern edge of the Black Forest area. Nearby places *Close (15 km): Waldshut-Tiengen, Schopfheim, Lörrach, Basel, Brugg AG, Aarau AG, Zürich, Schaffhausen SH, St. Blasien, Todtmoos, Freiburg i.Br., Konstanz. History The history of the city dates back to the early 6th Century, when Saint Fridolin founded Säckingen Abbey and a church. Around 1200 most of the city was destroyed in a huge fire. Afterwards, construction began in the middle of the town on a Gothic cathedral, called t ... [...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 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 Waldshut (district) Baden Hotzenwald {{Waldshut-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Herrischried
Herrischried 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 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 Baden Waldshut (district) Hotzenwald {{Waldshut-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Rhine
The High Rhine (german: Hochrhein) is the name used for the part of the Rhine that flows westbound from Lake Constance to Basel. The High Rhine begins at the outflow of the Rhine from the Untersee in Stein am Rhein and turns into the Upper Rhine in Basel. In contrast to the Alpine Rhine and Upper Rhine, the High Rhine flows mostly to the west. The section is marked by Rhine-kilometers 0 to 165, measurements beginning at the outflow of the Obersee at the Old Rhine Bridge in Constance. It is the first of four sections (High Rhine, Upper Rhine, Middle Rhine, Lower Rhine) of the Rhine between Lake Constance and the North Sea. In the western part, the Rhine marks the border between Germany and Switzerland, while in the eastern part, Switzerland owns areas north of the Rhine and surrounds the popular German holiday resort of Büsingen am Hochrhein. The term ''High Rhine'' was introduced by scientists in the 19th century. Above all geologists tried to differentiate the High Rhine () ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bernau Im Schwarzwald
Bernau is a municipality in the district of Waldshut in Baden-Württemberg in Germany. Geography Bernau is located in a high valley in the southern Black Forest, south of the Feldberg and west of the Schluchsee. Bernau includes the valley Bernauer Alb, a source stream of the Alb, and extends from 800 meters above sea level up to 1415 meters high. Neighboring communities The municipality is bordered to the north by the municipality of Feldberg, in the east by Menzenschwand and the city of St. Blasien, in the south of Ibach, in the southwest of Todtmoos and on the west by the city of Todtnau in the district of Lörrach. Weather The annual rainfall is 1919 mm. The driest month is September; most precipitation falls in December. In the wettest month, rain falls about 1.9 times more than the driest month. The temperatures are quite cool with -2.5 °C in January and 13.9 °C in July, and in the morning lower temperatures than on the Feldberg in Bernau are us ... [...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] |
Palaeozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but eve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Migmatite
Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian 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 pegmatitic, aplitic, 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 prograde metamorphism, when partial melting occurs in metamorphic paleosome. Components 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, incoherently folded veins ( ptygmatic folds).Recommendations by the IUGS Subcommission on the Systematics of M ... [...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] |
Rickenbach (Hotzenwald)
Rickenbach is the name of several places: Germany * Rickenbach, Baden-Württemberg Switzerland * Rickenbach, Basel-Landschaft * Rickenbach, Lucerne * Rickenbach, Schwyz * Rickenbach, Solothurn * Rickenbach, Thurgau Rickenbach is a municipality in the district of Münchwilen in the canton of Thurgau in Switzerland. History Rickenbach is first mentioned in 754 as ''Richinbach''. The Abbey of St. Gall acquired land in Rickenbach during the 8th century. The ... * Rickenbach, Zürich {{geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
