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Feuersteinklippe
The Feuersteinklippe is a rock formation in the Harz National Park in central Germany and the landmark of the nearby village of Schierke. The Feuersteinklippe is a butte made of granite, not flint (Feuerstein = "firestone" or flint) as the name suggests. It shows the spheroidal weathering typical of the Harz region. The striking rock formation is located at a height of 690 metres and is surrounded by woods. It lies to the north of Schierke station. The name Feuersteinklippe is derived from the Schierker Feuersteinwiesen (Schierke Feuerstein meadows) that lie to the southeast, which in turn were named after the cultic fires or signal beacons originally lit at this spot. An information board on the rocks recalls the visit of Goethe and the painter, Georg Melchior Kraus, who spent time here on 4 September 1784 in geological studies. The well-known herbal liqueur, Schierker Feuerstein, which is made in Schierke, is named after the rocks. The label portrays the rock formation. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schierke Feuersteinklippe 2010
Schierke is a village and a former municipality in the Harz district, in the German state of Saxony-Anhalt. Since 1 July 2009, it is part of the town Wernigerode. Situated within the Harz mountain range in the valley of the river Bode, at the rim of the Harz National Park, it is mainly a tourist resort, especially for hiking and all kinds of winter sports. Geography Location The winter sport and climatic spa of Schierke lies in the High Harz mountains, southeast of their highest summit, the Brocken. It is situated in the Harz/Saxony-Anhalt Nature Park and borders on the Harz National Park in the north. Situated 600 to 650 m above sea level in the valley of the Cold Bode, the parish of Schierke has an area of 40.1 km² and a population of 713 (as at 31 December 2007). Today Schierke again is a popular place to start or finish a walk to the Brocken massif via the '' Goetheweg'' or the ''Glashüttenweg''. It has bus service and access to the Brocken Railway, whose s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schierke
Schierke is a village and a former municipality in the Harz district, in the German state of Saxony-Anhalt. Since 1 July 2009, it is part of the town Wernigerode. Situated within the Harz mountain range in the valley of the river Bode, at the rim of the Harz National Park, it is mainly a tourist resort, especially for hiking and all kinds of winter sports. Geography Location The winter sport and climatic spa of Schierke lies in the High Harz mountains, southeast of their highest summit, the Brocken. It is situated in the Harz/Saxony-Anhalt Nature Park and borders on the Harz National Park in the north. Situated 600 to 650 m above sea level in the valley of the Cold Bode, the parish of Schierke has an area of 40.1 km² and a population of 713 (as at 31 December 2007). Today Schierke again is a popular place to start or finish a walk to the Brocken massif via the ''Goetheweg'' or the ''Glashüttenweg''. It has bus service and access to the Brocken Railway, whos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schierke Station
Schierke station (german: Bahnhof Schierke) is the railway station in the village of Schierke operated by the Harz Narrow Gauge Railways on the Brocken Railway in the Harz Mountains of central Germany. Schierke itself lies as the foot of the highest mountain in the Harz, the Brocken, and is located in the borough of Wernigerode in the federal state of Saxony-Anhalt. History The station, which is located at a height of 687 metres above sea level, was opened on 20 June 1898 and has been in continuous use as a railway station ever since. On the completion of the line up to the Brocken on 4 October 1898, trains to the highest mountain in North Germany, which were predominantly used by tourists, called at Schierke station. Because Brocken station was not served in winter due to heavy snowfalls, trains always terminated in Schierke from 16 October to 29 April. Not until the German Winter Sports Championships in spring 1950 did trains run to the Brocken in winter as well. As a result ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harzklippen
This is a list of rock formations in the Harz. They are known as the Harzklippen (literally "Harz crags" or "Harz cliffs") in German, which is the collective name for the, mainly, granite rock outcrops, crags and tors in the Harz mountains of Germany. Most of them have the status of a natural monument. The following list contains an alphabetically-sorted selection of rock formations in the Harz with - where known - their height in metres (m) above sea level, referenced to Normalnull (NN): * Achtermannstor (max. c. 900 m), on the Achtermannshöhe, near Braunlage, Lower Saxony * Ackertklippe, near Königshütte, Saxony-Anhalt * Adlerklippen (max. c. 340 m), in the valley of the Oker, near Goslar-Oker, Lower Saxony * Adlersklippen (see below: ''Teufelsmauer'') * Ahrentsklint (''Ahrentsklintklippe''; max. 822.4 m), on the Erdbeerkopf, near Schierke, Saxony-Anhalt * Altarklippen (max. c. 490 m), on the Heimberg, near Lautenthal, Lower Saxony * Anhaltin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schierker Feuerstein
Schierker Feuerstein is a German herbal liqueur, a half-bitters at a strength of 35% alcohol by volume (Alcohol proof, 61 degrees proof, or US 70 proof), originally produced in the village of Schierke, located in the Harz, Upper Harz region of Saxony-Anhalt, Germany. Due to its red-brown coloration, the liqueur is named after the so-called Feuersteinklippe, a rock formation near the village made of reddish granite. History The recipe was developed by the pharmacist Willy Drube (1880–1952), since 1908 proprietor of the chemist's ''Zum Roten Fingerhut'' in Schierke, and which was patented in 1924. Initially administered to Harz tourists, the liqueur soon became a big seller until production was discontinued during World War II. By the end of the war, Schierke belonged to the Soviet occupation zone. After the death of Willy Drube in 1952 and the migration of his descendants to West Germany, production was continued at Bad Lauterberg in the Lower Saxony, Lower Saxon part of the Har ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georg Melchior Kraus
Georg Melchior Kraus (26 July 1737, in Frankfurt am Main – 5 November 1806, in Weimar) was a German painter. He was a co-founder of the Weimar Princely Free Drawing School, together with Friedrich Justin Bertuch, in 1776. Life He was the sixth of nine children, five of whom died while infants. His parents, Cornelia and Johann, operated an inn called "Zur weissen Schlangen" (At the White Snakes) in Frankfurt. Cornelia died when he was eight, and Johann remarried that same year. From 1759 to 1762, he worked with Johann Heinrich Tischbein at his studio in Kassel, which was attached to the court of Frederick II, Landgrave of Hesse-Kassel. In 1762, he travelled to Paris to study with the engraver, Johann Georg Wille. While there, he also befriended the genre painter, Jean-Baptiste Greuze. After returning to Frankfurt, in 1766, he worked as a private drawing teacher. His notable students included Sophie von La Roche, Friedrich Heinrich Jacobi and Johann Wolfgang von Goethe. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goethe
Johann Wolfgang von Goethe (28 August 1749 – 22 March 1832) was a German poet, playwright, novelist, scientist, statesman, theatre director, and critic. His works include plays, poetry, literature, and aesthetic criticism, as well as treatises on botany, anatomy, and colour. He is widely regarded as the greatest and most influential writer in the German language, his work having a profound and wide-ranging influence on Western literary, political, and philosophical thought from the late 18th century to the present day.. Goethe took up residence in Weimar in November 1775 following the success of his first novel, '' The Sorrows of Young Werther'' (1774). He was ennobled by the Duke of Saxe-Weimar, Karl August, in 1782. Goethe was an early participant in the '' Sturm und Drang'' literary movement. During his first ten years in Weimar, Goethe became a member of the Duke's privy council (1776–1785), sat on the war and highway commissions, oversaw the reopening of silv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along streams and be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spheroidal 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formation
A rock formation is an isolated, scenic, or spectacular surface rock outcrop. Rock formations are usually the result of weathering and erosion sculpting the existing rock. The term ''rock formation'' can also refer to specific sedimentary strata or other rock unit in stratigraphic and petrologic studies. A rock structure can be created in any rock type or combination: * Igneous rocks are created when molten rock cools and solidifies, with or without crystallisation. They may be either plutonic bodies or volcanic extrusive. Again, erosive forces sculpt their current forms. * Metamorphic rocks are created by rocks that have been transformed into another kind of rock, usually by some combination of heat, pressure, and chemical alteration. * Sedimentary rocks are created by a variety of processes but usually involving deposition, grain by grain, layer by layer, in water or, in the case of terrestrial sediments, on land through the action of wind or sometimes moving ... [...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 near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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