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Rohrwald
The Rohrwald is a forest complex in the Weinviertel area of Lower Austria. With a total area of approx. 24 sq km (9 sq mi), it represents the third largest closed forest complex in the district of Korneuburg after the Tulln Basin-Danube floodplains and the Ernstbrunn Forest. The Rohrwald extends over the municipalities Harmannsdorf, Leobendorf, Leitzersdorf and Niederhollabrunn, whereby the largest part lies in the cadastral municipality Rückersdorf. The Rohrwald is located on a foothill of the flysch zone at the edge of the Korneuburg Basin and is therefore crossed by several streams, which is rather untypical for the Weinviertel. In the Weinviertel, which is poorly forested and intensively used for agricultural purposes, the Rohrwald has a high ecological value and an essential function as a local recreation area. Geology Geologically, the western peaks of the Rohrwald - the Waschberg and the Michelberg (Haselbach) - which are no longer forested and thus provide a goo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burg Kreuzenstein
Burg Kreuzenstein is a castle near Leobendorf in Lower Austria, Austria. Burg Kreuzenstein is above sea level. It was constructed on the remains of a medieval castle that had fallen into disrepair and was then demolished during the Thirty Years' War. Intended to be a family vault for the Wilczek family, it was rebuilt in the 19th century by Count Nepomuk Wilczek with money from the family's large Silesian coal mines. Kreuzenstein is interesting in that it was constructed out of sections of medieval structures purchased by the family from all over Europe to form an authentic-looking castle. Thus, the castle can be considered both a 'neo-' and 'original' medieval structure. The castle is sometimes used as a location for films. This castle is sometimes confused with the medieval castle Burg Liechtenstein, where the movie ''The Three Musketeers'' was filmed in 1993. Both castles used the same architect for restoration in the 19th century. Location The castle is located just north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Korneuburg
Korneuburg () is a town in Austria. It is located in the state Lower Austria and is the administrative center of the district of Korneuburg. Korneuburg is situated on the left bank of the Danube, opposite the city of Klosterneuburg, and is 12 km northwest of Vienna. It covers an area of 9.71 square km and, , there were 11,032 inhabitants. Korneuburg was originally a bank settlement associated with Klosterneuburg under the name Nivenburg. It was first mentioned in 1136, and in 1298 received the right to formal separation from Klosterneuburg. In 1938, the shipyard Korneuburg was integrated into the ''Hermann-Göring-Werke'', and significantly enlarged. In 1941, 16 barracks for Germans, forced laborers and prisoners of war were added. In 1945, the ''Red Army'' captured the shipyard. Military campaigns involving the city include the Battle of Vienna, the Thirty Years' War, the French Revolutionary Wars, and the Oil Campaign of World War II. The Korneuburg Shipyard is now the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falkenstein, Lower Austria
Falkenstein is a town in the district of Mistelbach in the Austrian state of Lower Austria Lower Austria (german: Niederösterreich; Austro-Bavarian: ''Niedaöstareich'', ''Niedaestareich'') is one of the nine states of Austria, located in the northeastern corner of the country. Since 1986, the capital of Lower Austria has been Sankt P .... It is home to Castle Falkenstein, a relatively intact castle ruin built in the 11th century. The ruin's German name is Burg Falkenstein ("Castle Falcon Stone"). Population References Cities and towns in Mistelbach District {{LowerAustria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Refuge Castle
A refuge castleCreighton, Oliver (2015). ''Early European Castles''. Bloomsbury. or refuge fort (german: Fliehburg, also ''Fluchtburg'', ''Volksburg'', ''Bauernburg'' or ''Vryburg'') is a castle-like defensive location, usually surrounded by ramparts, that is not permanently occupied but acts as a temporary retreat for the local population when threatened by war or attack. In former times such sites were also described as giant castles (German: ''Hünenburgen'') because their origin was ascribed to giants. History In Europe a multitude of large protohistoric sites surrounded by earthworks has been uncovered by archaeological excavations, many over 100 metres in diameter, that are understood to be refuge castles. Amongst ancient historical references to them are the refuge castles of the Gauls described by Caesar as ''oppida'', although they could also be permanent settlements. Similar ringwork (''Ringwall'') systems were built by the various Germanic and Slavic tribes, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Napoleonic Wars
The Napoleonic Wars (1803–1815) were a series of major global conflicts pitting the French Empire and its allies, led by Napoleon I, against a fluctuating array of European states formed into various coalitions. It produced a period of French domination over most of continental Europe. The wars stemmed from the unresolved disputes associated with the French Revolution and the French Revolutionary Wars consisting of the War of the First Coalition (1792–1797) and the War of the Second Coalition (1798–1802). The Napoleonic Wars are often described as five conflicts, each termed after the coalition that fought Napoleon: the Third Coalition (1803–1806), the Fourth (1806–1807), the Fifth (1809), the Sixth (1813–1814), and the Seventh (1815) plus the Peninsular War (1807–1814) and the French invasion of Russia (1812). Napoleon, upon ascending to First Consul of France in 1799, had inherited a republic in chaos; he subsequently created a state with stable financ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thirty Years' War
The Thirty Years' War was one of the longest and most destructive conflicts in European history The history of Europe is traditionally divided into four time periods: prehistoric Europe (prior to about 800 BC), classical antiquity (800 BC to AD 500), the Middle Ages (AD 500 to AD 1500), and the modern era (since AD 1500). The first early ..., lasting from 1618 to 1648. Fought primarily in Central Europe, an estimated 4.5 to 8 million soldiers and civilians died as a result of battle, famine, and disease, while some areas of what is now modern Germany experienced population declines of over 50%. Related conflicts include the Eighty Years' War, the War of the Mantuan Succession, the Franco-Spanish War (1635–1659), Franco-Spanish War, and the Portuguese Restoration War. Until the 20th century, historians generally viewed it as a continuation of the religious struggle initiated by the 16th-century Reformation within the Holy Roman Empire. The 1555 Peace of Augsburg atte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stockerau
Stockerau () is a town in the district of Korneuburg (district), Korneuburg in Lower Austria, Austria. Stockerau has 15,921 inhabitants, which makes it the largest town in the Weinviertel.https://statistik.at/wcm/idc/idcplg?IdcService=GET_PDF_FILE&RevisionSelectionMethod=LatestReleased&dDocName=103418 Stockerau is also called "Lenaustadt" (Lenau Town) because the Austrian poet Nikolaus Lenau often spent time with his grandparents here. Population Amenities Leisure facilities are various: wellness centre, sports centre with three gyms, judo and table tennis gym, skittle alley and football stadium. In addition there are indoor and outdoor tennis facilities. Stockerau offers a range of exhibitions, concerts, readings and singing evenings in the cultural centre "Belvedereschlößl". In the cellar of this castle, built in 16th century and revitalised by the town community in the year 1984, you will find the district museum. Between Stockerau and the Danube there is a large forest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Special Area Of Conservation
A Special Area of Conservation (SAC) is defined in the European Union's Habitats Directive (92/43/EEC), also known as the ''Directive on the Conservation of Natural Habitats and of Wild Fauna and Flora''. They are to protect the 220 habitats and approximately 1,000 species listed in annex I and II of the directive which are considered to be of European interest following criteria given in the directive. They must be chosen from the Sites of Community Importance by the member states and designated SAC by an act assuring the conservation measures of the natural habitat. SACs complement Special Protection Areas and together form a network of protected sites across the European Union called Natura 2000. This, in turn, is part of the Emerald network of Areas of Special Conservation Interest (ASCIs) under the Berne Convention. Assessment methodology in the United Kingdom Prior to being designated as a Special Area of Conservation (SAC), sites have been assessed under a two-stage process ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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