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Amselgrund
The Amselgrund ("Amsel Bottom") is the name given to the valley of the Grünbach stream in the heart of Saxon Switzerland in Eastern Germany. It runs from Niederrathen upstream to Rathewalde. The wild and romantic valley takes hikers through the Rathen rock basin with its bizarre rock formations. Its touristic high points are the lake of Amselsee and the Amsel Falls, that trickles over the grotto called the ''Amselloch''. The valley bottom that is densely wooded is surrounded by a backdrop of rocks. To the west tower the rocks of the ''Gansfelsen'', to the south the ''Feldsteine'' and the ''Türkenkopf'', and to the east rise the ''Honigsteine'' rocks with the striking Lokomotive. The middle of the valley bottom is dominated by the striking ''Talwächter''. Whilst the character of the valley profile in its upper reaches is rather ravine-like, between its entrance to the ''Schwedenlöcher'' and Niederrathen it is a steep valley. On the stream bed ripple marks may be seen. Above th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amselsee
The Amselsee (also ''Amselsee Rathen'') is a small reservoir in the spa town of Rathen in Saxon Switzerland. It is located in the Free State of Saxony in Eastern Germany. Reservoir To create the Amselsee in Saxon Switzerland, in 1934 a stream, the ''Grünbach'' (or ''Amselgrundbach''), the main waterbody in the Amselgrund valley, was impounded by the municipality of Rathen just above its confluence with the Wehlgrund that joins from the rights 1934. The dam is around five metres high. At 127 m above sea level the curved, narrow, roughly 550 m long trout pond is used in summer for boat rides (using slot machines!) as well as for fish breeding and also provides flood prevention. Round trips have been possible since 1969. The trout stock is sometimes mixed with American rainbow trout. Amongst the lakeside vegetation broad-winged damselflies or demoiselles may be seen. Dam The barrier is a straight gravity dam made of rubble stone masonry. It was built in 1934 and taken into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schwedenlöcher
The Schwedenlöcher is a gorge-like side valley of the Amselgrund near Rathen in Saxon Switzerland. History The deeply incised ravine was formed by the erosion of the soft sandstone. Its course follows the main direction of fissuring in the Elbe sandstone. Originally the Schwedenlöcher was an undeveloped gorge that was difficult to access and was known as the ''Blanker Grund''. When, during the Thirty Years’ War, the village of Rathewalde to the north was destroyed by Swedish soldiers in August 1639, the peasants of the region fled into the wild gorge and carried their possessions to safety. The gorge served as a refuge during later conflicts, such as in 1706 during the Great Nordic War, in 1813 during the Wars of Liberation and in 1945 during the last days of the Second World War. In the 1780s, the first tracks were made in the Schwedenlöchern in order to extract timber. This is recalled by several dates chiselled into the sandstone (1782, 1784, 1787). The first touri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rathen
Rathen is a village in the Elbe Sandstone Mountains, in Saxony, Germany, about southeast of Dresden. The village occupies both banks of the river Elbe and, as of 2020, has 339 inhabitants. Rathen is a popular tourist destination, the main sights are the Bastei cliffs, the Amselsee (a lake), and the outdoor theater ''"Felsenbühne Rathen"''. History Rathen was founded in the 13th century around 1261 as place for a castle fortress. During World War II, a subcamp of Flossenbürg concentration camp was located here. Tourism The state-recognised climatic spa of Rathen is not only the base for tours in the western part of Saxon Switzerland, but also for the world-famous Bastei rocks. Other popular destinations in the local Amselgrund valley are the lake of Amselsee and the Rathen Open Air Stage. There are a good 400 inhabitants on both sides of the Elbe, linked by the historic Rathen Ferry, which is a protected monument. In addition to the Old Mill of 1567, which was nearly d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amsel Falls
The Amsel Falls (german: Amselfall) are a waterfall in Saxon Switzerland in East Germany, roughly a kilometre north of the famous Bastei crags. As the ''Grünbach'' stream passes through a particularly narrow, gorge-like section of the Amselgrund valley it plunges over the largest step in the river bed - roughly 10 m high - forming a wide spray of water that pours over the ''Amselloch'', a collapsed cave. The roof of this cave was made of sandstone blocks that have collapsed. In the ravine and in the cave potholes and kolks bear witness to the meltwaters that coursed down into the River Elbe during earlier ice ages. The original stream (first mentioned in 1548) flowed almost entirely through the cave, but in the 19th century it had been diverted over the top of the cave to the cascade site. The waterfall was additionally, like the Lichtenhain Waterfall, arranged to flow through a small, controllable weir wicket in order to produce a stream-like torrent, in order to enhance it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bastei - Amselgrund Mit Amselsee, Lokomotive Und Dem Talwächter
The Bastei is a rock formation rising 194 metres above the Elbe River in the Elbe Sandstone Mountains of Germany. Reaching a height of 305 metres above sea level, the jagged rocks of the Bastei were formed by water erosion over one million years ago. They are situated near Rathen, not far from Pirna southeast of the city of Dresden, and are the major landmark of the Saxon Switzerland National Park. They are also part of a climbing and hiking area that extends over the borders into the Bohemian Switzerland (Czech Republic). The Bastei has been a tourist attraction for over 200 years. In 1824, a wooden bridge was constructed to link several rocks for the visitors. This bridge was replaced in 1851 by the present Bastei Bridge made of sandstone. The rock formations and vistas have inspired numerous artists, among them Caspar David Friedrich ("Felsenschlucht") The spa town of Rathen is the main base for visiting the Bastei; the town can be reached from Dresden by paddle steamer on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxon Switzerland
Saxon Switzerland (german: Sächsische Schweiz) is a hilly climbing area and national park around the Elbe valley south-east of Dresden in Saxony, Germany. Together with the Bohemian Switzerland in the Czech Republic it forms the Elbe Sandstone Mountains. Saxon Switzerland alone has some 1,000 climbing peaks, as well as several hollows. The area is popular with local and international climbers. The administrative district for the area is Sächsische Schweiz-Osterzgebirge. The fortress of Königstein is a well-known landmark. Etymology The German name for Saxon Switzerland, ''Sächsische Schweiz'', appeared in the 18th century. Two Swiss artists, Adrian Zingg and Anton Graff, were appointed in 1766 to the Dresden Academy of Art. They felt the landscape was reminiscent of their homeland, the Swiss Jura, and reported in their exchange of letters on the difference between their homeland and "Saxon Switzerland". Previously, the Saxon part of the Elbe Sandstone Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohnstein (Sächsische Schweiz)
Hohnstein () is a town located in the Sächsische Schweiz-Osterzgebirge district of Saxony, Germany. As of 2020, its population numbered a total of 3,262. Geography It is situated in Saxon Switzerland, 12 km east of Pirna, and 28 km southeast of Dresden (centre). It is dominated by its castle, standing on a sandstone rock. The municipal territory includes the villages (''Ortsteile'') of Cunnersdorf, Ehrenberg, Goßdorf, Lohsdorf, Rathewalde, Ulbersdorf and Waitzdorf. Gallery File:Stamps of Germany (DDR) 1985, MiNr 2976.jpg, 1985 stamp of the castle. File:Hohnstein - Burg und Stadt von Osten.JPG, View of the town and the castle. File:Hohnstein - Blick auf die Stadtkirche - geo-en.hlipp.de - 11321.jpg, Town's church File:Rathewalde_church.jpg, Church in Rathewalde File:Amselfall_2014.jpg, The Amsel Falls near Rathewalde See also *Hohnstein Castle (Saxon Switzerland) Hohnstein Castle (german: Burg Hohnstein) is a medieval castle in the village of the same name, Ho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lokomotive
The Lokomotive (German for "locomotive") is a striking climbing rock north of Kurort Rathen in Saxon Switzerland in Germany. The rock, which resembles a steam locomotive in appearance, is also known as ''Große Ruine'', is about 30 metres high and is divided into two parts: known as ''Lokomotive-Dom'' ("Locomotive Dome") and ''Lokomotive-Esse'' ("Locomotive Chimney"). The ridge between the two is called the ''Kesselgrat'' ("Boiler Ridge"), the rock teeth next to the Esse as ''Pfeife'' ("Whistle"). For a short time there was a weather vane on the dome in the shape of a wheel. The Lokomotive rises on the massif of the ''Honigsteine''. The Dome of the Lokomotive was first climbed in 1886 by Friedrich Hartmann and Robert Kappmeier. In the history of free climbing in Saxon Switzerland the climb of the Esse on 7 June 1903 by Albert Kunze and Oliver Perry-Smith was the first ascent of the Esse and the first step in climbing the open face. Until then climbers had focussed on chimneys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ripple Marks
In geology, ripple marks are sedimentary structures (i.e., bedforms of the lower flow regime) and indicate agitation by water ( current or waves) or wind. Defining ripple cross-laminae and asymmetric ripples * ''Current ripple marks'', ''unidirectional ripples'', or ''asymmetrical ripple marks'' are asymmetrical in profile, with a gentle up-current slope and a steeper down-current slope. The down-current slope is the angle of repose, which depends on the shape of the sediment. These commonly form in fluvial and aeolian depositional environments, and are a signifier of the lower part of the Lower Flow Regime. * Ripple cross-laminae forms when deposition takes place during migration of current or wave ripples. A series of cross-laminae are produced by superimposing migrating ripples. The ripples form lateral to one another, such that the crests of vertically succeeding laminae are out of phase and appear to be advancing upslope. This process results in cross-bedded unit ... [...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 relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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