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Earth Pyramids Of Ritten
The earth pyramids of Ritten (German: ''Erdpyramiden am Ritten''; it, Piramidi di terra del Renon ) are a natural monument that is located on the Ritten, a plateau not far from Bolzano in northern Italy. Earth pyramids are a fairly widespread phenomenon that exist in various locations, such as South Tyrol and Platten. The original name in this area for these earth pyramids is ''Lahntürme'', i.e., landslide towers.Cfr. Paul Stacul, ''Die erste Erwähnung der Südtiroler Erdpyramiden'' (''The first mention of the South Tyrolean earth pyramides''), in " Der Schlern", 51, 1977, pp. 675-678. They originate from glacial 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 shee ... rocks. The columns of the pyramids may be more or less elongated, and the higher they are, the thinner they ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ritten
Ritten (; it, Renon ) is a ''comune'' (municipality) in South Tyrol in northern Italy. Territory The community is named after the high plateau, elevation , the Ritten or the Renon, on which most of the villages are located. The plateau forms the southeast tip of the Sarntal Alps mountain range and is located between, and on average above the rivers Eisack and Talfer. Ritten lies directly northeast of Bolzano, settled on the "meeting point" of the above rivers. Ritten borders the following municipalities: Barbian, Bolzano, Kastelruth, Karneid, Völs, Jenesien, Sarntal and Villanders. As of 31 December 2016, Ritten had a population of 7,847.South Tyrol in figures 2008 by the Provincial Statistics Institute ASTAT, part of |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bolzano
Bolzano ( or ; german: Bozen, (formerly ); bar, Bozn; lld, Balsan or ) is the capital city of the province of South Tyrol in northern Italy. With a population of 108,245, Bolzano is also by far the largest city in South Tyrol and the third largest in historical Tyrol. The greater metro area has about 250,000 inhabitants and is one of the urban centers within the Alps. Bolzano is the seat of the Free University of Bozen-Bolzano, where lectures and seminars are held in English, German, and Italian. The city is also home to the Italian Army's Alpini High Command (COMALP) and some of its combat and support units. In the 2020 version of the annual ranking of quality of life in Italian cities, Bolzano was ranked joint first for quality of life alongside Bologna. Along with other Alpine towns in South Tyrol, Bolzano engages in the Alpine Town of the Year Association for the implementation of the Alpine Convention. The Convention aims to promote and achieve sustainable developme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoodoo (geology)
A hoodoo (also called a tent rock, fairy chimney, or earth pyramid) is a tall, thin spire of rock formed by erosion. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the elements. They generally form within sedimentary rock and volcanic rock formations. Hoodoos range in size from the height of an average human to heights exceeding a 10-story building. Hoodoo shapes are affected by the erosional patterns of alternating hard and softer rock layers. Minerals deposited within different rock types can cause hoodoos to have different colors throughout their height. Etymology In certain regions of western North America these rocky structures are called hoodoos. The name is derived from Hoodoo spirituality, in which certain natural forms are said to possess certain powers, but by the late 19th century, this spirituality became associated with bad luck. Prior to the English name for these geographic formations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earth Pyramids Of South Tyrol
The earth pyramids in South Tyrol are a special natural phenomenon that comes about in particular terrain, usually after a landslide or an unhinging of the earth. The main cause of the formation of earth pyramids is the continuous alternation of periods of torrential rain and drought. These phenomena, in particularly friable terrain, over the years, increasingly erode the ground and form such earth pyramids. Usually the pyramids are formed in terrain very well sheltered from wind so that they cannot be damaged by it. Moreover, the life of the earth pyramids is strongly dependent on the climate which reigns during the time in which it is shaped by the rock that covers it. There are several earth pyramids that can be safely visited. Among the most famous and admired the following are the most outstanding: * the earth pyramids of Ritten, a plateau above Bolzano, which are divided into three distinct groups near the villages Klobenstein, Oberbozen, and Unterinn * the earth pyrami ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earth Pyramids Of Platten
The earth pyramids of Platten (German: ''Erdpyramiden von Platten'' or ''Erdpyramiden bei Oberwielenbach''; it, Piramidi di Plata ) are earth pyramids located in Platten in the municipality of Percha, near Bruneck in South Tyrol, Italy. The erosion area is located at an altitude of 1550 to 1750 meters. What is so impressive about the pyramids of Platten is their wildness which reminds at the same time also of their fragility. The pyramids of Platten belong to the most beautiful natural monuments of South Tyrol such as the earth pyramids of Ritten and part of the earth pyramids of South Tyrol. They were described in a scientific manner for the first time by Karl Meusburger in 1914 .Karl Meusburger, ''Die Erdpyramiden bei Bruneck'' (''The earth pyramides near Bruneck'', in "Zeitschrift des Ferdinandeums für Tirol und Vorarlberg" (Journal of the Ferdinandeum The Tyrolean State Museum (german: Tiroler Landesmuseum), also known as the Ferdinandeum after Archduke Ferdinand, is lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Der Schlern
''Der Schlern'' (full German title: ''Der Schlern – Zeitschrift für Südtiroler Landeskunde''; en, The Schlern – Magazine for South Tyrolean Regional Studies) is a German-language monthly for the study of science, research, art and culture related to South Tyrol. First published on 1 January 1920, it is named after the Schlern, a characteristic mountain in the Dolomites. In 1938, it was forbidden by the Italian fascist regime as part of their Italianization of South Tyrol programme, but permitted again by the allied administration in 1946.Cf. Obermair (2013). ''Umbrüche – Übergänge – Chancen'', op. cit., pp. 273–4. The magazine is currently published in Bolzano Bolzano ( or ; german: Bozen, (formerly ); bar, Bozn; lld, Balsan or ) is the capital city of the province of South Tyrol in northern Italy. With a population of 108,245, Bolzano is also by far the largest city in South Tyrol and the third la ... by Athesia (formerly ''Tyrolia''). References Further ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Proven ... [...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] |
Geography Of South Tyrol
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). 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. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion Landforms
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 proceed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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