Lake Altaussee
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Lake Altaussee
Lake Altaussee, also known as Altausseersee, is a mountain lake located at the southwestern foot of the Totes Gebirge in the Styrian part of the Salzkammergut Mountains, Salzkammergut. It lies at 712 m above sea level. The center of the municipality of Altaussee is located on the western shore. The Altaussee Traun, which flows into the Danube via the Traun, serves as the outlet of the lake. The largely undeveloped shores and adjacent wetlands of Lake Altaussee provide habitats for numerous animal and plant species and have been under nature conservation since 1959. The Austrian Federal Forests own Lake Altaussee, which is a popular excursion destination due to its beautiful location. Every third year, the lake hosts the Daffodil Festival, Austria, Austria's largest flower festival. Geography The Totes Gebirge surround Lake Altaussee in a horseshoe shape. The Loser (mountain), Loser (1873m above sea level ) lies to the north, with steep flanks that drop sharply to the lakeshore. ...
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Styria
Styria ( ; ; ; ) is an Austrian Federal states of Austria, state in the southeast of the country. With an area of approximately , Styria is Austria's second largest state, after Lower Austria. It is bordered to the south by Slovenia, and clockwise, from the southwest, by the other Austrian states of Carinthia, Salzburg (federal state), Salzburg, Upper Austria, Lower Austria, and Burgenland. The state's capital is Graz, the second largest city in Austria after only Vienna. Name The March of Styria derived its name from the original seat of its ruling Otakars, Otakar dynasty: Steyr, in today's Upper Austria, which in turn derives its name from the namesake river of Steyr, stemming from the Celtic Stiria. In the native German the area is still called "Steiermark", while in English the Latin name "Styria" is used. Until the late 19th century however, the German name "Steyer", a slightly modernized spelling of Steyr, was also common. The ancient link between the city of Steyr and S ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ...
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Bad Aussee
Bad Aussee (; Central Bavarian: ''Bod Ossee'') is a town in the Austrian state of Styria, located at the confluence of the three sources of the Traun River in the Ausseerland region. Bad Aussee serves as the economic and cultural center of the Styrian part of the Salzkammergut lakes region. With a population of 4,862, the town is said to be the geographical midpoint of Austria, symbolized by a stone monument in the centre of town. Together with other Alpine towns Bad Aussee engages in the Alpine Town of the Year Association for the implementation of the Alpine Convention to achieve sustainable development in the Alpine Arc. Bad Aussee was awarded Alpine Town of the Year 2010. History Prehistoric artifacts were discovered in the nearby Salzofenhöhle cave. The town began to flourish in the Middle Ages, when salt works started operating in the late thirteenth century. Bad Aussee was designated a market town in 1295. The Romanesque and late Gothic Stadtpfarrkirche St. Paul ('' ...
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Bad Mitterndorf
Bad Mitterndorf () is a town in Salzkammergut in the Austrian state of Styria. Situated between Salzburg and Graz, it is a popular winter sports resort and also as a location for walking and cycling in the summer. Bad Mitterndorf is the site of two health spas with thermal baths, an outdoor swimming pool and other health amenities, cafés and leisure areas. The town hosts a children's club during the holidays. Bad Mitterndorf is also the location of one of the world's five ski flying hills, Kulm. The town is well placed for excursions to Hallstatt, Altaussee and its May narcissus festival, Bad Ischl and the Kaiservilla, and to Salzburg, 95 km away. Population Personalities Famous residents include the ski jumpers Hubert Neuper (1980 Olympic silver medallist and 1982 World Championship runner-up) and Wolfgang Loitzl (2009 World Champion and the 2008-9 Four Hills champion). Bad Mitterndorf is also the home town of Thomas Neuwirth aka Conchita Wurst, winner of the Eurovi ...
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Osterseen
Osterseen is a group of lakes in Bavaria, Germany, about 50 km (31 miles) south-south-west of Munich. At an elevation of 588 m (1,929 feet), its surface area is 223.55 ha (552.4 acres). Islands sorted by water body: Großer Ostersee (islands starting from North to South) * Holzau (6,1 hectares) * Marieninsel (2,3 hectares, Length 440 m in north–south orientation, width up to 80 metres)Historische Flurkarte
() im * Steigerinsel (0,45 ha), formerly ''Putzen Eila'' * Roseninsel (0,013 ha oder 130 m2, actually two very small islands) * Schwaigerinsel (0,75 ha, 40 m distance from western bank)


Frechensee

* unnamed island, c. 20 m distance from northern bank (0,09 ha) * unnamed island, c. 25 m from western bank (0,13 ha) ...
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Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to Semi-arid climate, semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where a flow of sediment or rocks emerge from a confined channel and are suddenly free to spread out in many directions. For example, many alluvial fans form when steep mountain valleys meet a flat plain. The transition from a narrow channel to a wide open area reduces the carrying capacity of flow and results in Deposition (geology), deposition of sediments. The flow can take the form of infrequent debris flows like in a landslide, or can be carried by an intermittent stream or creek. The reduction of flow is key to the formation of alluvial ...
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Bad Goisern Am Hallstättersee
Bad Goisern am Hallstättersee () is a market town in the Austrian state of Upper Austria in the Gmunden District, district of Gmunden. It is part of the Salzkammergut resort area. At the 2005 census Bad Goisern am Hallstättersee had a population of 7,578 inhabitants. History Bad Goisern am Hallstättersee is a town with a long history. It was first mentioned in the 13th century under the name "Gebisham". In 1931 Goisern became a spa town and in 1952 it became a market town. Since 1955 Goisern is called "Bad" Goisern (''Bad'' means bath in German and it is a title given by the government to cities with medicinal or Spa, thermal baths). A famous development is the "Goiserer Schuh", a good wearable mountain-shoe. Population Notable people * Franz Kain (1922–1997), Austrian writer and politician (KPO) * Herb Andress (1935–2004), born ''Herbert Andreas Greunz'', Austrian film and television actor * Ursula Haubner (born 1945), Austrian politician (FPÖ), older siste ...
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Ice Age
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 ice age called Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (''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, the term ''ice age'' is defined by the presence of extensive ice sheets in the northern and southern hemispheres. By this definition, the current Holocene epoch is an interglacial period of an ice age. The accumulation of anthropogenic greenhouse gases is projected to delay the next glacial period. History of research ...
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Lateral Moraines
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 are those 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'). in this case was derived from Provençal ...
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Terminal Moraine
A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from ...
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Oberalmer Formation
The Oberalmer Formation () is a geologic formation in Austria. It preserves fossils dated to the Cretaceous period. See also * List of fossiliferous stratigraphic units in Austria This is a list of fossiliferous stratigraphic units in Austria. __NOTOC__ List of fossiliferous stratigraphic units See also * List of fossiliferous stratigraphic units in Europe ** List of fossiliferous stratigraphic units in Germany ** ... References External links * Cretaceous System of Europe Cretaceous Austria Geologic formations of Austria {{Cretaceous-stub ...
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