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Danube-Günz Interglacial
The Danube-Gunz interglacial (), Danube-Gunz warm period (''Donau-Günz-Warmzeit''), often just Danube-Gunz, or also Uhlenberg interglacial (''Uhlenberg-Warmzeit'') are historical terms for a hypothetical warm period of the Pleistocene in the Alps, between the Danube and Gunz glacials. The interglacial was defined as the erosion phase that followed the Danube glacial and preceded the Gunz stage. It is therefore represented by the gap between the two depositions that are attributed to the two cold periods; in the type regions of the two glacial there are various depositions. In the area of the Iller-Lech Plateau they lie between the Lower Deckschotter (''Untere Deckschottern'') of the Zusam Plateau and the Intermediate Deckschotter (''Zwischenschottern''); in the region of the Salzach Glacier between the ''Eichwald Schotter'' and the Older Deckenschotter (''Ältere Deckenschottern''); and the area of Traun and Enns between the ''Prägünz Schotter'' and the Older Deckenschotter. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warm Period
An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age. The current Holocene interglacial began at the end of the Pleistocene, about 11,700 years ago. Pleistocene During the 2.5 million years of the Pleistocene, numerous glacials, or significant advances of continental ice sheets, in North America and Europe, occurred at intervals of approximately 40,000 to 100,000 years. The long glacial periods were separated by more temperate and shorter interglacials. During interglacials, such as the present one, the climate warms and the tundra recedes polewards following the ice sheets. Forests return to areas that once supported tundra vegetation. Interglacials are identified on land or in shallow epicontinental seas by their paleontology. Floral and faunal remains of species pointing to temperate climate and indicating a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from 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 () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alps
The Alps () are some of the highest and most extensive mountain ranges in Europe, stretching approximately across eight Alpine countries (from west to east): Monaco, France, Switzerland, Italy, Liechtenstein, Germany, Austria and Slovenia. The Alpine arch extends from Nice on the western Mediterranean Sea, Mediterranean to Trieste on the Adriatic Sea, 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 thrust fault, thrusting and Fold (geology), 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 82 peaks higher than List of Alpine four-thousanders, . The altitude and size of the range affect the climate in Europe; in the mountain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danube Glacial
Danube or Donau is a timespan in the glacial history of the Alps. Danube is currently regarded to have started approximately 1.8 million years ago, at the start of the Calabrian age of the international geochronology. It ended approximately one million years ago. Deep sea core samples have identified approximately 20 glacial cycles during Danube. History of the term The Danube glaciation, Donau glaciation () or the Danube Glacial (''Donau-Glazial'') was named by Barthel Eberl in 1930 after the River Danube. It did not appear in the traditional, quadripartite ice age schema of the Alps by Albrecht Penck. The Danube was the oldest glaciation in the Alps for which there was evidence outside of the Iller-Lech region. Danube Stage was thought to be preceded by the Biber-Danube interglacial and followed by the Danube-Günz interglacial. The 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission firmly places Danube (Donau) in the Calabrian and illustra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gunz Glacial
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 (, 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 2016 version of the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 procee ... [...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 concept is similar to type site in archaeology. 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, Finland * Kimberlite: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iller-Lech Plateau
The Iller-Lech Plateau (), 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. Sub-divisions The sub- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zusam
The Zusam () is a river in Bavaria, Germany and a right tributary of the Danube. Its source is just north of the village of Könghausen, in the Unterallgäu district of Bavaria. It flows north for approximately 97 km, before converging into the Danube near the town of Donauwörth Donauwörth (; ) is a town and the capital of the Donau-Ries district in Swabia, Bavaria, Germany. It is said to have been founded by two fishermen where the rivers Danube (Donau) and Wörnitz meet. The city is part of the scenic route called "R .... Towns and villages along the Zusam include Obergessertshausen, Memmenhausen, Muttershofen, Ziemetshausen, Dinkelscherben, Fleinhausen, Zusmarshausen, Zusamzell, Wertingen, Frauenstetten, and Buttenwiesen. References Rivers of Bavaria Tributaries of the Danube Bodies of water of Günzburg (district) Rivers of Germany {{Bavaria-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Traun (Donau)
Traun () is a river in the Austrian state of Upper Austria. Its source is in the Totes Gebirge mountain range in Styria. It flows through the Salzkammergut area and the lakes Hallstätter See and Traunsee. The Traun is a right tributary of the Danube, which it meets near the city of Linz. Other towns along the river are Bad Aussee, Bad Ischl, Gmunden, Wels and Traun. The Traun is long, and has a basin area of . Its average discharge at the mouth is . Until the late 19th century, it was only possible to reach Hallstatt (at the Hallstätter See) by boat or via narrow trails. However, this secluded and inhospitable landscape nevertheless counts as one of the first places of human settlement due to the rich sources of natural salt, which was mined for thousands of years, originally in the shape of hearts. Some of Hallstatt's oldest archaeological finds, such as a shoe-last celt – a long thin stone tool used to fell trees and to work wood – date back to around 5000 B.C. One of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enns (river)
The Enns () is a southern tributary of the river Danube in Austria, joining northward at the city of Enns. It forms much of the border between the states of Lower Austria and Upper Austria. The Enns spans , in a flat-J-shape. It flows from its source near the village Flachau, generally eastward through Radstadt, Schladming, and Liezen, then turns north near Hieflau, to flow past Weyer and Ternberg through Steyr, and further north to the Danube at Enns (''see map in References''). "Karte-Enns" (river map in German), RadTouren.at (Austria), May 2009, webpage: (236kb). Name It was known in Latin as ''Anisus'' or ''Anasus'', of uncertain origin; Anreiter et al. tried to link it to an Indo-European *''on''- and the hydronymic suffix *''-is-''. Later sources call it ''Ensa'' or ''Enisa''. Others have linked it to Upper Danubian Vasconic *''an'', "water." Another possible link is Greek ᾰ̓νῠστός (''anystos'', "useful"). The West Slavic languages have different name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine Glacier
The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance Lake Constance (, ) refers to three bodies of water on the Rhine at the northern foot of the Alps: Upper Lake Constance (''Obersee''), Lower Lake Constance (''Untersee''), and a connecting stretch of the Rhine, called the Seerhein (). These .... References Glaciers of Switzerland Rhine Former glaciers of Europe Last Glacial Period {{switzerland-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
