Schwedenlöcher
   HOME
*



picture info

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 Elbe Sandstone Mountains#Geology, 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 German Campaign of 1813, 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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Schwedenlöcher (Sächsische Schweiz) Um 1900 (01-2)
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 Elbe Sandstone Mountains#Geology, 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 German Campaign of 1813, 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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Schwedenlöcher Bei Rathen - Nationalpark Sächsische Schweiz 20
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 tou ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Rathen Und Elbsandsteingebirge Asv2022-08 Img24
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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


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 the ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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]  


picture info

Schwedenturm (rock)
The Schwedenturm ("Sweden Tower") in East Germany is a 35-metre-high rock formation made of sandstone in the hills of Saxon Switzerland near the spa town of Rathen and the famous Bastei rocks. From the car park for the Bastei, a path runs towards Schwedenlöcher. The Schwedenturm is situated on the right just before the entrance to a narrow ravine. Because it lies in the Saxon Switzerland Climbing Region the free-standing pinnacle may be used for climbing. Currently there are 14 different routes up the rock. It was here that the first grade Xb route in the mountain range was successfully climbed, route 6 (''Versuch''), by Bernd Arnold. The Schwedenturm was first climbed in 1905 by Rudolf Fehrmann Rudolf Fehrmann (22 June 1886 – 1947), a German, was a pioneer rock climber at Elbsandsteingebirge near Dresden. Climbing career He began climbing at the age of 17 and was soon at the leading edge of the fledgling sport. He and Oliver Perry-Sm ... and his brother Arymund. Exter ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Bastei (rock)
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 the ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Canyons And Gorges Of Germany
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Landforms Of Saxon Switzerland
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Rudolf Fehrmann
Rudolf Fehrmann (22 June 1886 – 1947), a German, was a pioneer rock climber at Elbsandsteingebirge near Dresden. Climbing career He began climbing at the age of 17 and was soon at the leading edge of the fledgling sport. He and Oliver Perry-Smith, an American college student and fellow climber living in Dresden, became as close as brothers and formed a team which pushed the limits of risk and difficulty on the steep sandstone spires, making many first ascents. Early on, Fehrmann exerted leadership in both climbing ethics and environmental protection. He imagined the purest of climbing routes as "great lines", ascending directly up steep faces and cracks and sometimes presenting considerable difficulties, and he encouraged the use of rope-soled slippers and a minimum of metal protective devices in order to avoid destroying the fragile rock. In 1903, Fehrmann began climbing on the Schrammsteine rocks. Before long, he became one of the best mountain climbers in Saxon Switzerland ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Saxon Switzerland Climbing Area
Saxon Switzerland (german: Sächsische Schweiz) is the largest and one of the best-known climbing regions in Germany, located in the Free State of Saxony. The region is largely coterminous with the natural region of the same name, Saxon Switzerland, but extends well beyond the territory of the National Park within it. It includes the western part of the Elbe Sandstone Mountains and is the oldest non-Alpine climbing region in Germany. Its history of climbing dates back to the first ascent in modern times of the Falkenstein by Bad Schandau gymnasts in 1864. Currently, there are over 1,100 summits with more than 17,000 climbing routes in the Saxon Switzerland area. Climbing in Saxon Switzerland Climbing in Saxon Switzerland is characterized by a strong traditional climbing ethic and a number of peculiarities rarely found in other climbing regions, or at least not to the same extent. An exception are Czech sandstone climbing regions, where similar rules apply. Climbers must obs ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Rockfall
A rockfall or rock-fallWhittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984. . is a quantity/sheets of rock that has fallen freely from a cliff face. The term is also used for collapse of rock from roof or walls of mine or quarry workings. "A rockfall is a fragment of rock (a block) detached by sliding, toppling, or falling, that falls along a vertical or sub-vertical cliff, proceeds down slope by bouncing and flying along ballistic trajectories or by rolling on talus or debris slopes." Alternatively, a "rockfall is the natural downward motion of a detached block or series of blocks with a small volume involving free falling, bouncing, rolling, and sliding". The mode of failure differs from that of a rockslide. Causal mechanisms Favourable geology and climate are the principal causal mechanisms of rockfall, factors that include intact condition of the rock mass, discontinuities within the rockmass, weathering susceptibility, ground and surface water, ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]