Günz-Haslach Interglacial
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Günz-Haslach Interglacial
The Gunz-Haslach interglacial (german: Günz-Haslach-Interglazial) and the Gunz-Haslach warm period (''Günz-Haslach-Warmzeit'') are historical terms for a hypothetical warm period of the Pleistocene in the Alpine region, between the Gunz and Haslach glaciations. The interglacial was defined as the erosion phase which follows the Günz and precedes the Haslach Glacial Stage. It thus corresponds to the stratigraphic gap between the Zeil gravels (''Zeiler Schotter'') in Swabia and Haslach gravels (''Haslacher Schotter'') northeast of the Rhine Glacier. Modern research has found that the old glacial terms correspond to many glacial cycles, as identified by marine isotope stages (MIS), making the term Gunz-Haslach superfluous. The term is not used in the 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission. See also * Timeline of glaciation There have been five or six major ice ages in the history of Earth over the past 3 billion years. The La ...
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Warm Period
Warm, WARM, or Warmth may refer to: * A somewhat high temperature * Kindness Music * ''Warm'' (The Lettermen album), 1967, and the title song * ''Warm'' (Johnny Mathis album), 1958, and the title song * ''Warm'' (Herb Alpert album), 1969 * ''Warm'' (Jeff Tweedy album), 2018 * ''Warmer'' (Randy VanWarmer album), 1979 * ''Warmer'' (Jeff Tweedy album), 2019 * "Warm", a song by Majid Jordan from ''Majid Jordan'', 2016 * "Warm", a song by Charli XCX featuring Haim from '' Charli'', 2019 * "Warmer", a song by Bea Miller from '' Chapter Two: Red'' and ''Aurora'', 2017 * "Warmth", by C418 from '' Minecraft - Volume Beta'', 2013 Other uses * ''Warm.'', taxonomic author abbreviation of Eugenius Warming (1841–1924), Danish botanist * WARM (foundation), an international foundation working on contemporary conflicts * WARM (AM), a radio station licensed to Scranton, Pennsylvania, United States * WARM-FM, a radio station (103.3 FM) licensed to York, Pennsylvania, United States * Wartime ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), 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 Great American Interchang ...
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Alps
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ...
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Gunz Glacial
Gunz may refer to: Games * '' GunZ: The Duel'', a 2005 South Korean online third-person shooting game * '' GunZ 2'', a 2011 South Korean fighting video game, sequel to ''GunZ: The Duel'' Places * Günz, a river in Bavaria, Germany ** Östliche Günz, or "eastern Günz," a river in Bavaria, Germany ** Westliche Günz, or "western Günz," a river in Bavaria, Germany * Günz Glacial Stage, name for an early Pleistocene stage used in the Alps Music * '' Gunz n' Butta'', a 2011 collaborative album by Cam'ron and Vado * Lord Tariq and Peter Gunz, American rap duo * Young Gunz, American rap duo People * Cory Gunz (born 1987), American rapper from The Bronx, New York City, New York * Gabriele Günz (born 1961), retired East German high jumper * (born 1946), German entrepreneur See also * Gun (other) A gun is an object that propels a projectile through a hollow tube, primarily as weaponry. Gun(s) may also refer to: Implements * Cannon * Artillery * Deluge gun * ...
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Haslach Glaciation
The Haslach glaciation (german: Haslach-Kaltzeit), Haslach Glacial Stage (''Haslach-Glazial''), Haslach Complex (''Haslach-Komplex'') and Haslach Ice Age (''Haslach-Eiszeit'') are historical terms for a cold period of the Pleistocene epoch. Haslach was not included in the traditional glacial schema of the Alps by Albrecht Penck and Eduard Brückner. The glacial stage was first described around 1981 by A. Schreiner and R. Ebel. Its type region is the Haslach Gravels (''Haslach-Schotter'') in the area of the Riss-Iller-Lech Plateau. The Haslach cold period was thought to be preceded by the Günz-Haslach interglacial and followed by the Haslach-Mindel Interglacial. The name Haslach is absent from the 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission. See also * Timeline of glaciation There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, it ...
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Erosion (geology)
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 ...
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Günz Glacial Stage
Gunz, Günz or Gunz Complex is a timespan in the glacial history of the Alps. It started approximately one million years ago and ended about 370 000 years ago. Some sources put the end at 480 000 years ago. Deep sea core samples have identified approximately 5 glacial cycles of varying intensity during Gunz. History of the term The name Gunz glaciation, Gunzian glaciation or Günz glacial stage (german: Günz-Kaltzeit, also ''Günz-Glazial'', ''Günz-Komplex'' and ''Günz-Eiszeit'') goes back to Albrecht Penck and Eduard Brückner, who named this ice age after the River Günz in their multi-volume work, ''Die Alpen im Eiszeitalter'' ("The Alps in the Ice Age Period") which was published between 1901 and 1909. Its type region is the Iller-Lech Plateau. It is the oldest glaciation of the Pleistocene in the traditional, quadripartite glacial classification of the Alps. The Günz was thought to follow the Danube-Günz interglacial and was ended by the Günz-Haslach interglacial. The ...
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Haslach Glacial Stage
The Haslach glaciation (german: Haslach-Kaltzeit), Haslach Glacial Stage (''Haslach-Glazial''), Haslach Complex (''Haslach-Komplex'') and Haslach Ice Age (''Haslach-Eiszeit'') are historical terms for a cold period of the Pleistocene epoch. Haslach was not included in the traditional glacial schema of the Alps by Albrecht Penck and Eduard Brückner. The glacial stage was first described around 1981 by A. Schreiner and R. Ebel. Its type region is the Haslach Gravels (''Haslach-Schotter'') in the area of the Riss-Iller-Lech Plateau. The Haslach cold period was thought to be preceded by the Günz-Haslach interglacial and followed by the Haslach-Mindel Interglacial. The name Haslach is absent from the 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission. See also * Timeline of glaciation There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its l ...
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Swabia
Swabia ; german: Schwaben , colloquially ''Schwabenland'' or ''Ländle''; archaic English also Suabia or Svebia is a cultural, historic and linguistic region in southwestern Germany. The name is ultimately derived from the medieval Duchy of Swabia, one of the German stem duchies, representing the territory of Alemannia, whose inhabitants interchangeably were called '' Alemanni'' or '' Suebi''. This territory would include all of the Alemannic German area, but the modern concept of Swabia is more restricted, due to the collapse of the duchy of Swabia in the thirteenth century. Swabia as understood in modern ethnography roughly coincides with the Swabian Circle of the Holy Roman Empire as it stood during the Early Modern period, now divided between the states of Bavaria and Baden-Württemberg. Swabians (''Schwaben'', singular ''Schwabe'') are the natives of Swabia and speakers of Swabian German. Their number was estimated at close to 0.8 million by SIL Ethnologue as of 2 ...
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Rhine Glacier
The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance. References Glaciers of Switzerland Rhine {{switzerland-glacier-stub ...
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Marine Isotope Stage
Marine isotope stages (MIS), marine oxygen-isotope stages, or oxygen isotope stages (OIS), are alternating warm and cool periods in the Earth's paleoclimate, deduced from oxygen isotope data reflecting changes in temperature derived from data from deep sea core samples. Working backwards from the present, which is MIS 1 in the scale, stages with even numbers have high levels of oxygen-18 and represent cold glacial periods, while the odd-numbered stages are lows in the oxygen-18 figures, representing warm interglacial intervals. The data are derived from pollen and foraminifera (plankton) remains in drilled marine sediment cores, sapropels, and other data that reflect historic climate; these are called proxies. The MIS timescale was developed from the pioneering work of Cesare Emiliani in the 1950s, and is now widely used in archaeology and other fields to express dating in the Quaternary period (the last 2.6 million years), as well as providing the fullest and best data ...
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Timeline Of Glaciation
There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its latest phase being the Quaternary glaciation, in progress since 2.58 million years ago. Within ice ages, there exist periods of more severe glacial conditions and more temperate conditions, referred to as glacial periods and interglacial periods, respectively. The Earth is currently in such an interglacial period of the Quaternary glaciation, with the last glacial period of the Quaternary having ended approximately 11,700 years ago. The current interglacial is known as the Holocene epoch.Walker, M., Johnsen, S., Rasmussen, S. O., Popp, T., Steffensen, J.-P., Gibbard, P., Hoek, W., Lowe, J., Andrews, J., Bjo¨ rck, S., Cwynar, L. C., Hughen, K., Kershaw, P., Kromer, B., Litt, T., Lowe, D. J., Nakagawa, T., Newnham, R., and Schwander, J. 2009Formal definition and dating of the GSSP (Global Stratotype Section and Point) for ...
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