Reichenbach (Hornberg)
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Reichenbach (Hornberg)
Reichenbach is a village in the municipality of Hornberg in the Black Forest in Germany. The territory of the town of Hornberg very small in comparison with its villages and restricted mainly to the valley bottom of the Gutach stream and the lower region of the Reichenbach valley. The village of Reichenbach covers the largest area in the municipality. Geography and geology Reichenbach is a dispersed settlement of around 650 inhabitants and covers the valleys east and west of Hornberg. In the east is the actual valley of the Reichenbach and those of the Schwanenbach, Schonenbächle and their side valleys. In the west the Offenbach- und Frombach valleys and side valleys belong to Reichenbach. The highest elevation in Reichenbach is the Windkapf with a height of 928 metres above Normalnull. The mountain range here consists mainly of granite. In the parish there are numerous woolsack rocks, of which the ''Igellochfelsen'' is the best known. In the eastern part of the parish, ...
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Hornberg
Hornberg is a town in the Ortenaukreis, in western Baden-Württemberg, Germany. It is situated in the Black Forest, 35 km southeast of Offenburg, and 25 km northwest of Villingen-Schwenningen. Sons and daughters of the town * (born 1948), physician (head of the radiology department of the hospital Konstanz), theologian and writer * Wilhelm Hausenstein (1882–1957), writer, art critic and cultural historian, journalist and diplomat *Friedrich Jeckeln (1895–1946), Nazi SS officer and Police Leader executed for war crimes * Thomas Schäuble (1948–2013), German politician ( CDU), Director of the Baden State Brewery Rothaus, brother of Wolfgang Schäuble Personalities who were active in Hornberg * Rochus Misch (1917–2013), bodyguard and telephone operator for Adolf Hitler; had a business for painters in Hornberg before the war * Wolfgang Schäuble Wolfgang Schäuble (; born 18 September 1942) is a German lawyer, politician and statesman whose political ...
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Black Forest
The Black Forest (german: Schwarzwald ) is a large forested mountain range in the state of Baden-Württemberg in southwest Germany, bounded by the Rhine Valley to the west and south and close to the borders with France and Switzerland. It is the source of the Danube and Neckar rivers. Its highest peak is the Feldberg with an elevation of above sea level. Roughly oblong in shape, with a length of and breadth of up to , it has an area of about 6,009 km2 (2,320 sq mi). Historically, the area was known for forestry and the mining of ore deposits, but tourism has now become the primary industry, accounting for around 300,000 jobs. There are several ruined military fortifications dating back to the 17th century. History In ancient times, the Black Forest was known as , after the Celtic deity, Abnoba. In Roman times (Late antiquity), it was given the name ("Marcynian Forest", from the Germanic word ''marka'' = "border"). The Black Forest probably represented the bo ...
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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 ...
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Gutach (Kinzig)
Gutach is a river of Baden-Württemberg, Germany. It passes through Triberg im Schwarzwald and Gutach (Schwarzwaldbahn), and flows into the Kinzig near Hausach. The Triberg Waterfalls are formed by the Gutach. 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, tr ... References Rivers of Baden-Württemberg Rivers of the Black Forest Rivers of Germany {{BadenWürttemberg-river-stub ...
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Dispersed Settlement
A dispersed settlement, also known as a scattered settlement, is one of the main types of settlement patterns used by landscape historians to classify rural settlements found in England and other parts of the world. Typically, there are a number of separate farmsteads scattered throughout the area. A dispersed settlement contrasts with a nucleated village. It can be known as main human settlements. The French term ''bocage'' is sometimes used to describe the type of landscape found where dispersed settlements are common. In addition to Western Europe, dispersed patterns of settlement are found in parts of Papua New Guinea, as among the Gainj, Ankave, and Baining tribes. It is also frequently met with in nomadic pastoral societies. In Ghana, Kumbyili in the northern region is also an example of a dispersed settlement England In England, dispersed settlements are often found in the areas of ancient enclosure outside the central region—for example, Essex, Kent and the West Cou ...
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Side Valley
Side valleys and tributary valleys are valleys whose brooks or rivers flow into greater ones. Upstream, the valleys can be classified in an increasing order which is equivalent to the usual orographic order: the tributaries are ordered from those nearest to the source of the river to those nearest to the mouth of the river. A confluence is where two or more tributaries or rivers flow together. Orographic order (e.g. Humber) In the orographic classification (order of rivers) the tributary river has order ''n+1'', if ''n'' describes the primary (or main) river. A river which flows directly into the ocean (e.g. the English rivers Thames or Humber) has the orographic order n=1, the River Ouse n=2, the Wharfe n=3 and so on. Geomorphology The term "side valley" is used for ''higher order valleys'' near mountains (example above: the Pennines), as opposed to lower valleys that do not have a strong relief. This is because the " main stem river" (into which the secondary river flo ...
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Normalnull
("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 1878 reference heights were taken from the Amsterdam Ordnance Datum and transferred to the New Berlin Observatory in order to define the . has been defined as a level going through an imaginary point 37.000 m below . When the New Berlin Observatory was demolished in 1912 the reference point was moved east to the village of Hoppegarten (now part of the town of Müncheberg, Brandenburg, 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 ...).S. German: ''Was ist "Normal-Null"?''. In: ''Physikalische Blätter'' 1958, vol 14, issue 2, p. ...
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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 ...
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Woolsack Weathering
Spheroidal weathering is a form of chemical weathering that affects jointed bedrock and results in the formation of concentric or spherical layers of highly decayed rock within weathered bedrock that is known as ''saprolite.'' When saprolite is exposed by physical erosion, these concentric layers peel (spall) off as concentric shells much like the layers of a peeled onion. Within saprolite, spheroidal weathering often creates rounded boulders, known as ''corestones'' or ''woolsack'', of relatively unweathered rock. Spheroidal weathering is also called onion skin weathering, concentric weathering, spherical weathering, or woolsack weathering.Fairbridge, RW (1968) ''Spheroidal Weathering.'' in RW Fairbridge, ed., pp. 1041–1044, The Encyclopedia of Geomorphology, Encyclopedia of Earth Sciences, vol. III. Reinhold Book Corporation, New York, New York. Ollier, C.D. (1971). ''Causes of spheroidal weathering. ''Earth-Science Reviews 7:127–141.Neuendorf, KKE, JP Mehl Jr., and JA J ...
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Fohrenbühl
Fohrenbühl is a mountain of Baden-Württemberg, 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 .... Mountains and hills of Baden-Württemberg Mountains and hills of the Black Forest Mountain passes of the Black Forest Mountain passes of Baden-Württemberg {{BadenWürttemberg-geo-stub ...
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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 ...
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Villages In Baden-Württemberg
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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