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Erdmannshöhle
The Erdmannshöhle is a stalactite or flowstone cave in the village Hasel between Schopfheim and Wehr, 20 km east of Lörrach in Baden-Württemberg in Germany.Black ForestThe Erdmannshöhle in Hasel/ref> Name The word Erdmannshöhle is comparable to earth man's hole and composed of the three German nouns Erde (earth), Mann (man) and Höhle (cave). Erdmann is also a German forename and a surname. As a forename it was often given to show the connection with the earth. In the Baroque the Republic of Venice sent mineralogical prospectors to the countries north of the Alps to look for the raw materials which were necessary for glassmaking. These prospectors were called "Venetians" everywhere else and only in the Black Forest they were called "Stumm-Männle" (meaning "dumb little men", because they did not speak with the local people) were mostly very small, wore an ankle-long tunic with a hood like the cowl of a monk and carefully avoided contact. These mysterious migrants ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hasel, Germany
Hasel is a municipality in the district of Lörrach in Baden-Württemberg in Germany. The placename was first mentioned in a document dated 7 June 820 in which the monastery of St. Gallen lent its property in "Hasalaho" as a fief. In all probability the placename refers to a place of jurisdiction and execution of the Alamanni that was enclosed by hazel pales. The German word "Hasel" which is the placename means the same as the English "Hazel". It has been said that this is the location of The Dwarves' Cavern which was supposedly once home to many dwarves. This legend gives the cavern its name. The preceding statement may refer to the Erdmannshöhle where the legend is, however, not about dwarfs (which is "Zwerge" in German German(s) may refer to: * Germany, the country of the Germans and German things **Germania (Roman era) * Germans, citizens of Germany, people of German ancestry, or native speakers of the German language ** For citizenship in Germany, see also Ge ...) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diminutive
A diminutive is a word obtained by modifying a root word to convey a slighter degree of its root meaning, either to convey the smallness of the object or quality named, or to convey a sense of intimacy or endearment, and sometimes to belittle something or someone. A ( abbreviated ) is a word-formation device used to express such meanings. A is a diminutive form with two diminutive suffixes rather than one. Purpose Diminutives are often employed as nicknames and pet names when speaking to small children and when expressing extreme tenderness and intimacy to an adult. The opposite of the diminutive form is the augmentative. In some contexts, diminutives are also employed in a pejorative sense to denote that someone or something is weak or childish. For example, one of the last Western Roman emperors was Romulus Augustus, but his name was diminutivized to "Romulus Augustulus" to express his powerlessness. Formation In many languages, diminutives are word forms that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of The Black Forest
Geography (from Ancient Greek ; combining 'Earth' and 'write', literally 'Earth writing') is the study of the lands, features, inhabitants, and phenomena of Earth. Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. Geography has been called "a bridge between natural science and social science disciplines." Origins of many of the concepts in geography can be traced to Greek Eratosthenes of Cyrene, who may have coined the term "geographia" (). The first recorded use of the word γεωγραφία was as the title of a book by Greek scholar Claudius Ptolemy (100 – 170 AD). This work created the so-called "Ptolemaic tradition" of geography, which included "Ptolemaic cartographic theory." ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Show Caves In Germany
Show or The Show may refer to: Competition, event, or artistic production * Agricultural show, associated with agriculture and animal husbandry * Animal show, a judged event in the hobby of animal fancy ** Cat show ** Dog show ** Horse show ** Specialty show, a dog show which reviews a single breed *Fashion show, showcase of clothing and/or accessories *Show, an artistic production, such as: ** Concert ** Game show ** Radio show ** Talk show ** Television show ** Theatre production * Trade show Arts, entertainment, and media Films * ''Show'' (film), a 2002 film * ''The Show'' (1922 film), starring Oliver Hardy * ''The Show'' (1927 film), directed by Tod Browning * ''The Show'' (1995 film), a hip hop documentary * ''The Show'' (2017 film), an American satirical drama * ''The Show'' (2020 film), a British mystery film Albums * ''Show'' (The Cure album), 1993 * ''Show'' (The Jesus Lizard album), 1994 * ''The Show'' (eMC album), 2008 * ''The Show'' (Niall Horan albu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Germany
Caves or caverns are natural voids under the Earth's surface. Caves often form by the weathering of rock and often extend deep underground. Exogene caves are smaller openings that extend a relatively short distance underground (such as rock shelters). Caves which extend further underground than the opening is wide are called endogene caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganisms, pressure, and atmospheric influences. Isotopic dating techniques can be applied to cave sediments, to determine the time ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactite
A stalactite (, ; , ) is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension (chemistry), suspension, or is capable of being melting, melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch (resin), pitch, sand, Geyserite, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Formation and type Limestone stalactites The most common stalactites are speleothems, which occur in limestone caves. They form through Deposition (geology), deposition of calcium carbonate and other minerals, which is precipitated from mineralized water Solution (chemistry), solutio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; ) is a sequence of sedimentary rock, sedimentary rock strata (a lithostratigraphy, lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the three-part Germanic Trias (that gives the Triassic its name) lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk ("mussel-chalk") consists of a sequence of limestone and Dolomite (rock), dolomite Bed (geology), beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the layers of rock. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system (stratigraphy), system. The name indicates a characteristic feature of the unit, name ... [...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] |
Wiese (river)
The Wiese () is a river, 57.8 kilometres long, and a Orographic left and right-hand tributary of the Rhine in southwest Germany and northwest Switzerland. From its source in Baden-Württemberg in the Southern Black Forest on the mountain of the Feldberg (Black Forest), Feldberg, it flows for a short distance though the county of Breisgau-Hochschwarzwald and then mainly across Landkreis Lörrach, Lörrach and through numerous settlements including the county town of Lörrach. After crossing the international border, the lower reaches of the river pass through the canton of Basel-Stadt, mainly through the city of Basel and through its district of Kleinbasel before emptying into the Upper Rhine. The valley of the Wiese, which drains a drainage basin, catchment of 455 square kilometres, is called the ''Wiesental, Black Forest, Wiesental'' or Wiese Valley; it is oriented roughly towards the south-west. Its largest tributary is the Little Wiese (''Kleine Wiese'') which approaches fro ... [...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] |
Buntsandstein
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphy, lithostratigraphic and allostratigraphy, allostratigraphic unit (a sequence of rock strata) in the Subsurface (geology), subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series (stratigraphy), series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup (geology), Supergroup. The Buntsandstein is similar in age, sedimentary facies, facies and lithology with the Bunter (geology), 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 chronostratigraphy, chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies ... [...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] |
