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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cold Period
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called ''interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albrecht Penck
Albrecht Penck (25 September 1858 – 7 March 1945) was a German geographer and geologist and the father of Walther Penck. Biography Born in Reudnitz near Leipzig, Penck became a university professor in Vienna, Austria, from 1885 to 1906, and in Berlin from 1906 to 1927. There he was also the director of the Institute and Museum for Oceanography by 1918. He dedicated himself to geomorphology and climatology, and he raised the international profile of the Vienna school of physical geography. With Eduard Brückner, he coauthored ''Die Alpen im Eiszeitalter'', a work in which the two scientists identified the four ice ages of the European Pleistocene ( Gunz, Mindel, Riss, Würm); these being named after the river valleys that were the first indication of each glaciation. In 1886, he married the sister of the successful Bavarian regional writer Ludwig Ganghofer. In 1945, Penck died in Prague. In Vienna, he taught the Polish geographer Eugeniusz Romer and Ukrainian geographe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eduard Brückner
Eduard Brückner (29 July 1862 – 20 May 1927) was a geographer, glaciologist and climatologist. Biography He was born in Jena, the son of the Baltic-German historian Alexander Brückner and Lucie Schiele. After an education at the Karlsruhe gymnasium, beginning in 1881 he studied meteorology and physics at the University of Dorpat, graduating in 1885. He joined the Deutsche Seewarte (German Hydrographic Office) in Hamburg, then, following studies at Dresden and Munich, he became a professor at the University of Bern in 1888. The same year he married Ernestine Steine. In 1899, he was rector at the university. He moved back to Germany in 1904, becoming a professor at the University of Halle. Two years later in 1906, he was a professor at the University of Vienna. He died in Vienna. Professor Brückner was an expert on alpine glaciers and their effect upon the landscape. Between 1901–1909 he collaborated with German geographer and geologist Albrecht Penck to produce a three volum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Type Locality (geology)
Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified. If the stratigraphic unit in a locality is layered, it is called a stratotype, whereas the standard of reference for unlayered rocks is the type locality. The term is similar to the term type site in archaeology or the term type specimen in biology. Examples of geological type localities Rocks and minerals * Aragonite: Molina de Aragón, Guadalajara, Spain * Autunite: Autun, France * Benmoreite: Ben More (Mull), Scotland * Blairmorite: Blairmore, Alberta, Canada * Boninite: Bonin Islands, Japan * Comendite: Comende, San Pietro Island, Sardinia * Cummingtonite: Cummington, Massachusetts * Dunite: Dun Mountain, New Zealand. * Essexite: Essex County, Massachusetts, US * Fayalite: Horta, Fayal Island, Azores, Portugal * Harzburgite: Bad Harzburg, Germany * Icelandite: Thingmuli (Þingmúli), Iceland * Ijolite: Iivaara, Kuusamo, Finl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riss (river)
The Riss (german: Riß) is a small river in Baden-Württemberg, south-western Germany, right tributary of the Danube. Its source is in Upper Swabia, between Bad Waldsee and Bad Schussenried. It flows north, through the town of Biberach an der Riss. It then flows into the Danube one mile north of Rißtissen between Ehingen and Erbach, approximately 20 km upstream from Ulm. Its total length is approximately 50 km. The Riss gave its name to the Riss glaciation, an ice age. See also * List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach * Aalenbach * Ablach * Ach *Acher * Adelbach *Aich * Aid * Aischbach, tributary of the Kinzig * Aischbach, tributary of the Körsch *Aitrach, tributary of the Danube *Aitrach, tr ... References Rivers of Baden-Württemberg Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iller-Lech Plateau
The Iller-Lech Plateau (german: Donau-Iller-Lech-Platte), also known as the Upper Swabian Plateau (''Oberschwäbische Hochebene''), is one of the natural regions of Germany. Boundaries In the northwest the Iller-Lech Plateau borders on the Swabian Jura (unit D60 on the map) and, in the extreme northeast, on the Franconian Jura (unit D61 on the map). The boundary with these two natural regions is roughly formed by the course of the river Danube. In the east the Iller-Lech Plateau borders on the Lower Bavarian Upland and Isar-Inn Gravel Plateaus (unit D65 on the map). North of Augsburg its eastern boundary runs roughly parallel to state road 2035 (Augsburg-Pöttmes-Neuburg an der Donau), south of Augsburg east of the Lech, roughly between Mering, Geltendorf and Schongau. To the south the Southern Alpine Foreland (D66 on the map) borders on the Iller-Lech Plateau. The boundary between these two natural regions is partly formed by the terminal moraines of the Würm glaciation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haslach-Mindel Interglacial
The Haslach-Mindel interglacial (german: Haslach-Mindel-Interglazial) and the Haslach-Mindel warm period (''Haslach-Mindel-Warmzeit'') are historical terms for a hypothetical warm period of the Pleistocene in the Alpine region, between the Haslach and Mindel glacial stages. The interglacial was defined as the erosion phase which follows the Haslach and precedes the Mindel glacial stage. It thus corresponds to the stratigraphic gap between the Haslach beds (''Haslacher Schotter'') and the Tannheim-Laupheim gravels (''Tannheim-Laupheimer 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 Haslach-Mindel 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene Events
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 two reg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
