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Kreuzberg (Tempelhofer Berge)
The Kreuzberg (German for ''Cross Mountain'') is a hill in the Kreuzberg locality of Berlin, Germany, in former West Berlin. It rises about above the sea level. It was named by King Frederick William III of Prussia after the Iron Cross which crowns the top of the Prussian National Monument for the Liberation Wars, designed by Karl Friedrich Schinkel, on its inauguration on 30 March 1821. On 27 September 1921 the borough assembly of the VIth borough of Berlin decided to name the borough after the hill. The borough was subsequently downgraded to a locality in 2001. Other names for the hill Former names of the Kreuzberg were ''Sandberg'' (sand mountain), ''Runder Berg'' (1524) or ''Runder Weinberg'' (Round Mountain or Round Wine Mountain/Vineyard), ''Tempelhofer Berg'' and corrupted ''Templower Berg'' (both Tempelhof Mountain), ''Götzens Berg'' (1798) or ''Götzescher Berg'' (1818; both Götze's Mountain), ''Kreutzberg'' (1822, 1834) and ''Kreuzberg'' (1856). Since the 1850s the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otto Piltz
Otto Piltz (28 June 1846, Allstedt - 20 August 1910, Pasing) was a German genre painter and illustrator for ''Die Gartenlaube''. Life He was the son of a soap-maker. After an apprenticeship as a decorative painter in Halle, he studied at the Weimar Saxon-Grand Ducal Art School from 1866 to 1871. His teachers were Paul Thumann, Bernhard Plockhorst and Charles Verlat. During the 1870s, he worked at the artists' colonies in Kleinsassen and Willingshausen. He lived in Weimar until 1886, Berlin until 1889, then in Pasing until his death. In 1882, he was appointed a Professor by Grand Duke Charles Alexander. He became a member of the Munich Secession in 1893. He painted both urban and rural scenes but was especially successful at painting children. He also travelled throughout Thuringia, Hesse, Bavaria and the Tyrol, documenting the local costumes that were already beginning to disappear. He sometimes accompanied a young friend, Franz Marc, on painting excursions to Dachau. He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teltow Plateau
Teltow [] is both a geological plateau and also a historical region in the German states of Brandenburg and Berlin. As an historical region, the Teltow was one of the eight territories out of which the March of Brandenburg was formed in the 12th and 13th centuries. As a result of the (1239–1245) the question of territorial lordship of the newly created heart of the expanding march was finally decided here. Between 1835 and 1952 there was also a county, ; in addition a town immediately south of Berlin, in the present-day county of Potsdam-Mittelmark, bears the name Teltow. Geography and geology Boundary The Teltow is not a unified region, either from a historical or a landscape perspective. The present-day term is defined by an ice age plateau that consists mainly of ground moraine elements. Its natural northern border is defined by the range of the Tempelhofer Berge, among them the Kreuzberg rising to , along the southern bank of the Spree. To the east the borders are for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franciscan Cloister Church, Berlin
, image = FrancescoCoA PioM.svg , image_size = 200px , caption = A cross, Christ's arm and Saint Francis's arm, a universal symbol of the Franciscans , abbreviation = OFM , predecessor = , merged = , formation = , founder = Francis of Assisi , founding_location = , extinction = , merger = , type = Mendicant Order of Pontifical Right for men , status = , purpose = , headquarters = Via S. Maria Mediatrice 25, 00165 Rome, Italy , location = , coords = , region = , services = , membership = 12,476 members (8,512 priests) as of 2020 , language = , sec_gen = , leader_title = Motto , leader_name = ''Pax et bonum'' ''Peace and llgood'' , leader_title2 = Minister General , leader_name2 = ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franciscan
The Franciscans are a group of related Mendicant orders, mendicant Christianity, Christian Catholic religious order, religious orders within the Catholic Church. Founded in 1209 by Italian Catholic friar Francis of Assisi, these orders include three independent orders for men (the Order of Friars Minor being the largest contemporary male order), orders for women religious such as the Order of Saint Clare, and the Third Order of Saint Francis open to male and female members. They adhere to the teachings and spiritual disciplines of the founder and of his main associates and followers, such as Clare of Assisi, Anthony of Padua, and Elizabeth of Hungary. Several smaller Franciscan spirituality in Protestantism, Protestant Franciscan orders exist as well, notably in the Anglican and Lutheran traditions (e.g. the Community of Francis and Clare). Francis began preaching around 1207 and traveled to Rome to seek approval from Pope Innocent III in 1209 to form a new religious order. The o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Commandry (feudalism)
In the Middle Ages, a commandery (rarely commandry) was the smallest administrative division of the European landed properties of a military order. It was also the name of the house where the knights of the commandery lived.Anthony Luttrell and Greg O'Malley (eds.), ''The Countryside Of Hospitaller Rhodes 1306–1423: Original Texts And English Summaries'' (Routledge, 2019), p. 27. The word is also applied to the emoluments granted to a commander. They were the equivalent for those orders to a monastic grange. The knight in charge of a commandery was a commander. Etymology The word derives from French ''commanderie'' or ''commenderie'', from mediaeval Latin ''commendaria'' or ''commenda'', meaning "a trust or charge", originally one held ''in commendam''. "commandery , commandry, n." OED Online, Oxford University Press, December 2018, https://www.oed.com/view/Entry/36962. Accessed 9 December 2018. Originally, commandries were benefices, particularly in the Church, held ''in comm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knights Templar
, colors = White mantle with a red cross , colors_label = Attire , march = , mascot = Two knights riding a single horse , equipment = , equipment_label = , battles = The Crusades, including: , anniversaries = , decorations = , battle_honours = , commander1 = Hugues de Payens , commander1_label = First Grand Master , commander2 = Jacques de Molay , commander2_label = Last Grand Master , commander3 = , commander3_label = , notable_commanders = The Poor Fellow-Soldiers of Christ and of the Temple of Solomon ( la, Pauperes commilitones Christi Templique Salomonici), also known as the Order of Solomon's Temple, the Knights Templar, or simply the Templars, was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barnim Plateau
The Barnim Plateau is a plateau which is occupied by the northeastern parts of Berlin and the surrounding federal state of Brandenburg in Germany. Boundaries and Subdivision Boundaries The limits of the plateau are easily definable. The southern boundary is marked by the Berlin Valley, through which the River Spree flows. To the west, the boundary between Barnim and the Glien Plateau is marked by a north-south glacial valley. To the north and north east is the boundary with the Eberswald Valley, and in the east, Lubusz Land. Subdivision Traditionally the plateau is divided into the Upper and Lower Barnim, separated by a line running between Strausberg and Eberswalde. Typically, Lower Barnim does not reach higher than 80 metres above mean sea level (AMSL) whereas Upper Barnim is generally more than 100 metres AMSL. The highest point of the plateau is Semmelberg which stands at 157 metres AMSL. Settlements Until the growth of Berlin in the 19th century, Barnim was only spars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prenzlauer Berg
Prenzlauer Berg () is a locality of Berlin, forming the southerly and most urban district of the borough of Pankow. From its founding in 1920 until 2001, Prenzlauer Berg was a district of Berlin in its own right. However, that year it was incorporated (along with the borough of Weißensee) into the greater district of Pankow. From the 1960s onward, Prenzlauer Berg was associated with proponents of East Germany's diverse counterculture including Christian activists, bohemians, state-independent artists, and the gay community. It was an important site for the peaceful revolution that brought down the Berlin Wall in 1989. In the 1990s the borough was also home to a vibrant squatting scene. It has since experienced rapid gentrification. Geography Prenzlauer Berg is a portion of the Pankow district in northeast Berlin. To the West and Southwest it borders Mitte, to the South Friedrichshain-Kreuzberg, to the East Lichtenberg, and to the North Weißensee and Pankow. Geologically, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weichselian Glaciation
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (german: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (''Weichsel-Kaltzeit''), Weichselian glacial (''Weichsel-Glazial''), ''Weichselian Stage'' or, rarely, the Weichselian complex (''Weichsel-Komplex''). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ..., in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ground Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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