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Rochlitz - Blick Von Der Mulde Zum Schloss (02-3)
Rochlitz (; hsb, Rochlica) is a major district town (Große Kreisstadt) in the district of Mittelsachsen, in Saxony, Germany. Rochlitz is the head of the "municipal partnership Rochlitz" (Verwaltungsgemeinschaft Rochlitz) with its other members being the municipalities of Königsfeld, Saxony, Königsfeld, Seelitz and Zettlitz. Geography Location The town is situated on a bend of the river Zwickauer Mulde and at the foot of Rochlitzer Berg, 26 km northwest of Chemnitz and 45 km from Leipzig or Zwickau. Geology Rochlitz is situated in the Natural Region ''Sächsisches Lössgefilde'' ("Saxon Loess country") and its sub-region ''Mulde-Lösshügelland'' ("Mulde Loess hill country"). Rochlitzer Berg (ca. 349 m (Normalhöhennull, NHN)) is of Rotliegend volcanic origin (latest Carboniferous to Guadalupian) and consists to a large extent of so-called ''Rochlitzer Porphyr'', a Rhyolite, rhyolitic tuff or ignimbrite. Due to its colour and structure, this rock is used in re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rochlitz Castle
Rochlitz Castle or Rochlitz Palace (german: Schloss Rochlitz) lies in the west of the town of Rochlitz in the county of Mittelsachsen in the Free State of Saxony. It was built on the site of an imperial castle, erected in the second half of the 10th century, which fell into the possession of the Wettin margraves in 1143. Its appearance, which includes several Romanesque wings, is considerably influenced by its remodelling into a margravial '' schloss'' in the fourth quarter of the 14th century. Further conversions and additions followed at the end of the 15th and in the 16th centuries, when the castle became a secondary '' residenz'', dower house and hunting lodge for the Wettin family. The castle or palace was the residence for members of the Saxon princely house eight times. From the 18th century the castle served as an administrative centre (justice department and district court); in 1852 it became a gaol, which necessitated considerable alteration. The museum founded in 1892 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guadalupian
The Guadalupian is the second and middle series/ epoch of the Permian. The Guadalupian was preceded by the Cisuralian and followed by the Lopingian. It is named after the Guadalupe Mountains of New Mexico and Texas, and dates between 272.95 ± 0.5 – 259.1 ± 0.4 Mya. The series saw the rise of the therapsids, a minor extinction event called Olson's Extinction and a significant mass extinction called the end-Capitanian extinction event. The Guadalupian was previously known as the Middle Permian. Name and background The Guadalupian is the second and middle series or epoch of the Permian. Previously called Middle Permian, the name of this epoch is part of a revision of Permian stratigraphy for standard global correlation. The name "Guadalupian" was first proposed in the early 1900s, and approved by the International Subcommission on Permian Stratigraphy in 1996. References to the Middle Permian still exist. The Guadalupian was preceded by the Cisuralian and followed by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Theodoric I, Margrave Of Meissen
Theodoric I (11 March 1162 – 18 February 1221), called the Oppressed (''Dietrich der Bedrängte''), was the Margrave of Meissen from 1198 until his death. He was the second son of Otto II, Margrave of Meissen and Hedwig of Brandenburg. Biography Theodoric, called in German Dietrich, the younger son of Otto II, Margrave of Meissen, fell out with his brother, Albert the Proud, after his mother persuaded his father to change the succession so that Theodoric was given the Margraviate of Meissen and Albrecht (although the older son) the margraviate of Weissenfels. Albert took his father prisoner to try to make him return the succession to the way it had been. After Otto obtained his release by an order of the emperor Frederick I, he had only just renewed the war when he died in 1190. Albert then took back the Meissen margraviate from his brother. Theodoric attempted to regain the margraviate, supported by ''Landgraf'' Hermann I of Thuringia, his father-in-law. In 1195, however ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Margrave
Margrave was originally the medieval title for the military commander assigned to maintain the defence of one of the border provinces of the Holy Roman Empire or of a kingdom. That position became hereditary in certain feudal families in the Empire and the title came to be borne by rulers of some Imperial principalities until the abolition of the Empire in 1806 (e.g., Margrave of Brandenburg, Margrave of Baden). Thereafter, those domains (originally known as ''marks'' or ''marches'', later as ''margraviates'' or ''margravates'') were absorbed in larger realms or the titleholders adopted titles indicative of full sovereignty. History Etymologically, the word "margrave" ( la, marchio, links=no, ) is the English and French form of the German noble title (, meaning " march" or "mark", that is, border land, added to , meaning "Count"); it is related semantically to the English title " Marcher Lord". As a noun and hereditary title, "margrave" was common among the languages of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lusatia
Lusatia (german: Lausitz, pl, Łużyce, hsb, Łužica, dsb, Łužyca, cs, Lužice, la, Lusatia, rarely also referred to as Sorbia) is a historical region in Central Europe, split between Germany and Poland. Lusatia stretches from the Bóbr and Kwisa rivers in the east to the Pulsnitz (river), Pulsnitz and Black Elster rivers in the west, and is located within the German states of Saxony and Brandenburg as well as in the Polish voivodeships of Lower Silesian Voivodeship, Lower Silesia and Lubusz Voivodeship, Lubusz. Lusatia's central rivers are the Spree (river), Spree and the Lusatian Neisse, which constitutes the border between Germany and Poland since 1945 (Oder–Neisse line). The Lusatian Mountains (part of the Sudetes), separate Lusatia from Bohemia (Czech Republic) in the south. Lusatia is traditionally divided into Upper Lusatia (the hilly southern part) and Lower Lusatia (the flat northern part). The areas east and west along the Spree in the German part of Lusatia a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dedi III, Margrave Of Lusatia
Dedi III (german: Dedo), nicknamed ''the Fat'' ( – 16 August 1190), a member of the House of Wettin, was Margrave of Lusatia from 1185 until his death. Life Dedo was a younger son of the Wettin margrave Conrad I of Meissen and his wife Luitgard of Ravenstein. From 1144, he administered the lordship of Groitzsch as heir apparent of the late Count Henry of Groitzsch (d. 1135), and also as an adopted son of his aunt Bertha (d. 1143), Henry's sister and Groitzsch heiress. When Margrave Conrad retired in 1156, the extended Wettin estates were divided and Dedi formally received the County of Groitzsch and the Lordship of Rochlitz, with jurisdiction over the Bishopric of Naumburg. Dedi participated in five campaigns of the Hohenstaufen emperor Frederick Barbarossa to Italy. In 1177, he served as Frederick's envoy to Pope Alexander III and swore, on Frederick's behalf, to uphold the Treaty of Venice, which ended the schism between pope and emperor. Back in Germany, Dedi appea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ford (crossing)
A ford is a shallow place with good footing where a river or stream may be crossed by wading, or inside a vehicle getting its wheels wet. A ford may occur naturally or be constructed. Fords may be impassable during high water. A low-water crossing is a low bridge that allows crossing over a river or stream when water is low but may be treated as a ford when the river is high and water covers the crossing. Description A ford is a much cheaper form of river crossing than a bridge, and it can transport much more weight than a bridge, but it may become impassable after heavy rain or during flood conditions. A ford is therefore normally only suitable for very minor roads (and for paths intended for walkers and horse riders etc.). Most modern fords are usually shallow enough to be crossed by cars and other wheeled or tracked vehicles (a process known as "fording"). Fords may be accompanied by stepping stones for pedestrians. The United Kingdom has more than 2,000 fords, and mos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sorbs
Sorbs ( hsb, Serbja, dsb, Serby, german: Sorben; also known as Lusatians, Lusatian Serbs and Wends) are a indigenous West Slavic ethnic group predominantly inhabiting the parts of Lusatia located in the German states of Saxony and Brandenburg. Sorbs traditionally speak the Sorbian languages (also known as "Wendish" and "Lusatian"), which are closely related to Czech language, Czech, Polish language, Polish, Kashubian language, Kashubian, Silesian language, Silesian, and Slovak language, Slovak. Upper Sorbian and Lower Sorbian are officially recognized minority languages in Germany. Due to a gradual and increasing Cultural assimilation, assimilation between the 17th and 20th centuries, virtually all Sorbs also spoke German by the early 20th century. In the newly created German Empire, German nation state of the late 19th and early 20th centuries, policies were implemented in an effort to Germanize the Sorbs. These policies reached their climax under the Nazi Germany, N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slavs
Slavs are the largest European ethnolinguistic group. They speak the various Slavic languages, belonging to the larger Balto-Slavic language, Balto-Slavic branch of the Indo-European languages. Slavs are geographically distributed throughout northern Eurasia, mainly inhabiting Central Europe, Central and Eastern Europe, and the Balkans to the west; and Siberia to the east. A large Slavic minority is also scattered across the Baltic states and Central Asia, while a substantial Slavic diaspora is found throughout the Americas, as a result of immigration. Present-day Slavs are classified into East Slavs (chiefly Belarusians, Russians, Rusyns, and Ukrainians), West Slavs (chiefly Czechs, Kashubians, Poles, Slovaks and Sorbs) and South Slavs (chiefly Bosniaks, Bulgarians, Croats, Macedonians (ethnic group), Macedonians, Montenegrins, Serbs and Slovenes). The vast majority of Slavs are traditionally Christians. However, modern Slavic nations and ethnic groups are considerably dive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediments
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water ( fluvial processes), but also wind ( aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Town Hall (Leipzig)
Leipzig's Old Town Hall – which dominates the east side of the marketplace in Leipzig's district Mitte - is considered one of Germany's most important secular Renaissance buildings. At the rear is the Naschmarkt (Sweet market). The mayor and the municipal administration have been housed in the new town hall since 1905. Description The Old Town Hall is a landmark of Leipzig and is generally considered to be an extremely beautiful building. The impression of beauty comes from length, colour, uniformity and proportions. With two storeys and a length of more than 300 feet, the building would be long but not high, if there would not be the steep roof. The eaves edge is low, so the roof contributes significantly to the height. As far as its effect is concerned, it is receded into the background by the row of wall dormers (6 on the Marktplatz side, 7 on the Naschmarkt side) with their connecting horizontal lines. Compared to the length, the width of the house is also relatively ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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