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Dreistromstein
The Dreistromstein (Three Rivers Stone) is a three-sided obelisk that has marked the watershed of the Weser, Elbe and Rhine rivers in the Thuringian Forest since 1906. The base of the obelisk is made of stone typical of each of the river systems—Elbe: granite; Weser: greywacke; Rhein: quartz. Opposite the Dreistromstein is the Kleine Dreiherrenstein (Little Three Lords Stone) or Dreiherrenstein am Saarzipfel (Three Lords Stone at Saarzipfel) from 1733, which marks the border of the duchies of Saxe-Meiningen and Saxe-Hildburghausen and the principality A principality (or sometimes princedom) can either be a monarchical feudatory or a sovereign state, ruled or reigned over by a regnant-monarch with the title of prince and/or princess, or by a monarch with another title considered to fall under ... of Schwarzburg-Rudolstadt. See also * '' Dreiherrnstein'' Geography of Thuringia Thuringian Forest {{thuringia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dreistromstein - Panoramio
The Dreistromstein (Three Rivers Stone) is a three-sided obelisk that has marked the watershed of the Weser, Elbe and Rhine rivers in the Thuringian Forest since 1906. The base of the obelisk is made of stone typical of each of the river systems—Elbe: granite; Weser: greywacke; Rhein: quartz. Opposite the Dreistromstein is the Kleine Dreiherrenstein (Little Three Lords Stone) or Dreiherrenstein am Saarzipfel (Three Lords Stone at Saarzipfel) from 1733, which marks the border of the duchies of Saxe-Meiningen and Saxe-Hildburghausen and the principality A principality (or sometimes princedom) can either be a monarchical feudatory or a sovereign state, ruled or reigned over by a regnant-monarch with the title of prince and/or princess, or by a monarch with another title considered to fall under ... of Schwarzburg-Rudolstadt. See also * '' Dreiherrnstein'' Geography of Thuringia Thuringian Forest {{thuringia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dreiherrnstein
A ''Dreiherrenstein'' or ''Dreiherrnstein'' is the topographic name of a historical tripoint, especially in the German-speaking lands of central Europe, i.e. a place where the border of three princely territories met, together with any enclosures or border fortifications. The word means literally "Three Lords' Stone". Examples Examples of places where ''Dreiherrensteine'' are located include: * Boundary stone between the municipalities of Friesenhagen, Wenden and the town of Freudenberg. Es handelt sich um die former border of the Barony of Wildenburg with the kurkölnischen Duchy of Westphalia and the Principality of Nassau-Siegen. * Boundary stone in Medenbach, Wiesbaden, in the parish of "Wellinger" that once marked the borders of Nassau-Idstein, Electoral Mainz and the Hesse-Darmstadt. It bears the date 1730. * Boundary stone between the bishoprics of Münster, Osnabrück and Orange * Boundary stone in the municipality of Bellingen (Westerwald) on the border between Elec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weser
The Weser () is a river of Lower Saxony in north-west Germany. It begins at Hannoversch Münden through the confluence of the Werra and Fulda. It passes through the Hanseatic city of Bremen. Its mouth is further north against the ports of Bremerhaven and Nordenham. The latter is on the Butjadingen Peninsula. It then merges into the North Sea via two highly saline, estuarine mouths. It connects to the canal network running east-west across the North German Plain. The river, when combined with the Werra (a dialectal form of "Weser"), is long and thus, the longest river entirely situated within Germany (the Main, however, is the longest if the Weser and Werra are not combined). The Weser itself is long. The Werra rises in Thuringia, the German state south of the main projection (tongue) of Lower Saxony. Etymology "Weser" and "Werra" are the same words in different dialects. The difference reflects the old linguistic border between Central and Low German, passing through H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbe
The Elbe (; cs, Labe ; nds, Ilv or ''Elv''; Upper and dsb, Łobjo) is one of the major rivers of Central Europe. It rises in the Giant Mountains of the northern Czech Republic before traversing much of Bohemia (western half of the Czech Republic), then Germany and flowing into the North Sea at Cuxhaven, northwest of Hamburg. Its total length is . The Elbe's major tributaries include the rivers Vltava, Saale, Havel, Mulde, Schwarze Elster, and Ohře. The Elbe river basin, comprising the Elbe and its tributaries, has a catchment area of , the twelfth largest in Europe. The basin spans four countries, however it lies almost entirely just in two of them, Germany (65.5%) and the Czech Republic (33.7%, covering about two thirds of the state's territory). Marginally, the basin stretches also to Austria (0.6%) and Poland (0.2%). The Elbe catchment area is inhabited by 24.4 million people, the biggest cities within are Berlin, Hamburg, Prague, Dresden and Leipzig. Etymology Firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thuringian Forest
The Thuringian Forest (''Thüringer Wald'' in German), is a mountain range in the southern parts of the German state of Thuringia, running northwest to southeast. Skirting from its southerly source in foothills to a gorge on its north-west side is the Werra valley. On the other side of the Forest is an upper outcrop of the North German Plain, the Thuringian Basin, which includes the city Erfurt. The south and south-east continuation of the range is the highland often called the Thuringian-Vogtlandian Slate Mountains. Among scattered foothills at its northern foot are the towns Eisenach, Gotha, Arnstadt and Ilmenau. The town of Suhl sits in a slight dip on the range itself. In October 1806, Napoleon Bonaparte invaded Saxony with his "Grande Armée," fighting the Battle of Jena–Auerstedt near the wood. This battle, part of the War of the Fourth Coalition, is generally regarded as the basis of Napoleon's success over the Alliance. Geography and communications The Thuringia ... [...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] |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duchies
A duchy, also called a dukedom, is a medieval country, territory, fief, or domain ruled by a duke or duchess, a ruler hierarchically second to the king or queen in Western European tradition. There once existed an important difference between "sovereign dukes" and dukes who were ordinary noblemen throughout Europe. Some historic duchies were sovereign in areas that would become part of nation-states only during the modern era, such as happened in Germany (once a federal empire) and Italy (previously a unified kingdom). In contrast, others were subordinate districts of those kingdoms that had unified either partially or completely during the medieval era, such as France, Spain, Sicily, Naples, and the Papal States. Examples In France, several duchies existed in the medieval period, including Normandy, Burgundy, Brittany, and Aquitaine. The medieval German stem duchies (german: Stammesherzogtum, literally "tribal duchy," the official title of its ruler being ''Herzog'' or "duke") ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxe-Meiningen
Saxe-Meiningen (; german: Sachsen-Meiningen ) was one of the Saxon duchies held by the Ernestine line of the Wettin dynasty, located in the southwest of the present-day German state of Thuringia. Established in 1681, by partition of the Ernestine duchy of Saxe-Gotha among the seven sons of deceased Duke Ernst der Fromme (Ernest the Pious), the Saxe-Meiningen line of the House of Wettin lasted until the end of the German monarchies in 1918. History House of Wettin The Wettiner had been the rulers of sizeable holdings in today's states of Saxony, Saxony-Anhalt and Thuringia since the Middle Ages. In the '' Leipziger Teilung'' of 1485, the Wettiner were split into two branches named after their founding princes Albrecht and Ernst (''albertinisch'' and ''ernestinisch''). Thuringia was part of the Ernestine holdings of ''Kursachsen'' (the Electoral holdings of Saxony). In 1572, the branches Saxe-Coburg-Eisenach and Saxe-Weimar were established there. The senior line again split ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxe-Hildburghausen
Saxe-Hildburghausen () was an Ernestine duchy in the southern side of the present State of Thuringia in Germany. It existed from 1680 to 1826 but its name and borders are currently used by the District of Hildburghausen. History After the Duke of Saxe-Gotha, Ernest the Pious, died on 26 March 1675 in Gotha, the Principality was divided on 24 February 1680 among his seven surviving sons. The lands of Saxe-Hildburghausen went to the sixth son, who became Ernest II, the first Duke of Saxe-Hildburghausen. But the new Principality did not have complete independence. It had to depend on the higher authorities in Gotha for the matters of administration of its districts – the so-called "" – because Gotha was the residence of Ernest II's oldest brother, who ruled as Frederick I, Duke of Saxe-Gotha-Altenburg. Saxe-Hildburghausen did not become fully sovereign until 1702. In the beginning, the Principality had the District and city of Hildburghausen, the District and city of Heldbu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
