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Wildmoossee
The Wildmoossee is an aperiodic mountain lake, 3 kilometres west of Seefeld in Tirol near the village of Wildmoos in the market borough of Telfs. The lake lies in the area of the water-soluble main dolomite of the Seefeld Plateau at a height of 1,316 metres.Naturphänomen Wildmoossee und Lottensee - Tirol', tirol.at As a result the ground underneath contains chasms that reach up to the bottom of the lake. About every four years, so much groundwater builds up as a result of precipitation and snow meltwater that it is forced upwards out of the chasms under pressure and emerges spring-like at the surface, filling the lake basin. The highest water levels are usually reached in May. In late autumn, the lake empties itself again. This cycle can change due to the variable level of water resulting from variations in precipitation. The same karst Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is charact ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wildmoos (Telfs)
Wildmoos is an area in the central Inn valley in North Tyrol and a village in the municipality of Telfs in the district of Innsbruck Land. Geography Wildmoos lies beyond Innsbruck on the Seefeld Plateau above the Inn, at around 1260 , near Seefeld. The area encompasses just under 30 scattered houses; today most of the land is covered by the ''Seefeld-Wildmoos'' Golf Course and the alpine meadow of ''Wildmoosalm''. Nature The Wildmoos area is a large aquatic ecotope of about with two rarely appearing aperiodic lakes, the '' Lottensee'' and the ''Wildmoossee'', with a further bog and wetland area on the ''Wildalm''.FMOOR ''Wildmoosalm'' 70.721,04 m², FSON ''Gebiet um Wildmoosalm - Koellental'' 63.321,02 m² The two areas are separated by forest. They are both karst phenomena. Seefeld-Wildmoos Golf Course The region has been developed today into an 18-hole golf course A golf course is the grounds on which the sport of golf is played. It consists of a ser ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seefeld Plateau
The Seefeld Plateau (german: Seefelder Plateau) is a montane valley and basin landscape in the North Tyrolean Limestone Alps about 500 metres above the Inn valley in the Austrian state of Tyrol. The plateau covers the valley basin around the villages of Seefeld in Tirol and Scharnitz as well as the valley of ''Leutaschtal''. Location The Seefeld Plateau runs northwards from the edge of the Inn graben at the Zirler Berg. It lies at a height of around in the North Tyrolean Limestone Alps between the Wetterstein Mountains to the northwest, the Mieming Mountains to the west and the Karwendel to the east. The Seefeld Saddle (), a mountain pass and saddle south of Seefeld, forms a watershed, north of which the plateau drains towards the Isar and south of which it drains into the Inn. Geology and flora The dominant rocks of the Seefeld Plateaus are Wetterstein limestone and main dolomite with scattered occurrences of bituminous slate. A branch of the ice age Inn Glacie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seefeld In Tirol
Seefeld in Tirol is an old farming village, now a major tourist resort, in Innsbruck-Land District in the Austrian state of Tyrol (state), Tyrol with a local population of 3,312 (as of 1 January 2013). The village is located about northwest of Innsbruck on a plateau between the Wetterstein mountains and the Karwendel on a historic road from Mittenwald to Innsbruck that has been important since the Middle Ages. It was first mentioned in 1022 and since the 14th century has been a pilgrimage church, pilgrimage site, benefiting not only from the visit of numerous pilgrims but also from its stacking rights as a trading station between Augsburg and the Republic of Venice, Venice. Also since the 14th century, Tyrolean shale oil has been extracted in the area. Seefeld was a popular holiday resort even before 1900 and, since the 1930s, has been a well known winter sports area, winter sports centres and amongst the most popular tourist resorts in Austria. The municipality, which has been the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Groundwater
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, perma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artesian Well
An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer has trapped water, surrounded by layers of impermeable rock or clay, which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached. A well drilled into such an aquifer is called an ''artesian well''. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a ''flowing artesian well''. Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks, similar to how many newly tapped oil wells are pressurized. From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmospher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ..., in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyrol (Bundesland)
Tyrol (; german: Tirol ; it, Tirolo) is a state (''Land'') in western Austria. It comprises the Austrian part of the historical Princely County of Tyrol. It is a constituent part of the present-day Euroregion Tyrol–South Tyrol–Trentino (together with South Tyrol and Trentino in Italy). The capital of Tyrol is Innsbruck. Geography The state of Tyrol is separated into two parts, divided by a strip. The larger territory is called North Tyrol (''Nordtirol'') and the smaller area is called East Tyrol (''Osttirol''). The neighbouring Austrian state of Salzburg stands to the east, while on the south Tyrol has a border with the Italian province of South Tyrol (Trentino-Alto Adige/Südtirol) which was part of the Austro-Hungarian Empire before the First World War. With a land area of , Tyrol is the third-largest state in Austria. Tyrol shares its borders with the federal state of Salzburg in the east and Vorarlberg in the west. In the north, it adjoins to the German state of Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chasm
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the point ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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