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Traungold Cave
Traungold Cave (german: link=no, Traungoldhöhle, no. 1623/231 in the Austrian Cave Register) is a cave which has provided shelter and storage space to the Cambridge University Caving Club during their expeditions to Austria. Entrance E and F are two ends of a large stone arch, which has been developed into a bivouac shelter known as the "Stone Bridge." The location allows easy access to Steinbrücken Cave Steinbrücken Cave (german: Steinbrückenhöhle, "Stone bridge cave", no. 1623/204 in the Austrian cave register) was discovered by the Cambridge University Caving Club on the Loser Plateau in 1999. It is part of the large Schwarzmooskogel cave sy ... for exploration trips. Over the years the floor has been remodelled by filling in holes with stones to create more flat ground, and during this process the connection between entrances E and F and the rest of the cave was filled in. Food must be stored off the floor in hammocks to avoid becoming infested by mice. Between expediti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bivouac Shelter
A bivouac shelter is any of a variety of improvised camp site, or shelter that is usually of a temporary nature, used especially by soldiers, or people engaged in backpacking, bikepacking, scouting, or mountain climbing. It may often refer to sleeping in the open with a bivouac sack, but it may also refer to a shelter constructed of natural materials like a structure of branches to form a frame, which is then covered with leaves, ferns, and similar material for waterproofing and duff (leaf litter) for insulation. Modern bivouacs often involve the use of one- or two-man tents but may also be without tents or full cover. In modern mountaineering the nature of the bivouac shelter will depend on the level of preparedness, in particular whether existing camping and outdoor gear may be incorporated into the shelter. A bivouac shelter is colloquially known as a bivvy (also spelled ''bivy'' or ''bivvi'' or ''bivi''). Etymology The word ''bivouac'' is French and ultimately derives from a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loser Plateau
The Loser Plateau (also referred-to as the Loser-AugstEck plateau) is part of the Totes Gebirge mountain range in the Salzkammergut of Austria. It is most easily accessed up a toll road from the town of Altaussee. It is a Nature Reserve, notable for its caves and unspoilt alpine Karst ecosystem. Hunting permits are issued to control Chamois. The central plateau area is relatively flat, at an altitude of 1500-1600m, rising gently to the north and east, and covering about 4 km2. The whole massif is approximately 12 km2. The area drops steeply on all sides, and is bounded to the SE by path 234 from the Wildenseehutte down to Altausseer See, to the south by the lake itself, then to the SW by the road to Blaa-Alm. The Western edge is marked by the valley of Grüne Bichl, and the northern limit is the ridge crest of Schönberg, then a rather ill-defined line back to the Wildenseehütte. Recently its southern (Loser) face has been heavily developed for skiing. Access to the a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambridge University Caving Club
The Cambridge University Caving Club was founded in 1949. The club organizes single rope technique (SRT) training, social events, and weekend caving trips as well as longer expeditions. Currently, annual expeditions are carried out to the Ardèche region of France for sport. Between 1988 and 1997 there were annual Christmas expeditions to Majorca, Spain. The main summer expedition, which has been going on nearly every year since 1976, has been to the Loser Plateau, in the Totes Gebirge Mountains, Austria. Since around 1980 the base camp has been in Bad Aussee. Notable caves that have been discovered and explored include Steinbrückenhöhle (1999–present), Kaninchenhöhle (1988–1998), Stellerweghöhle (1972–1982). Former members of the club have founded Hong Meigui cave exploration society of China. See also * University of Bristol Spelæological Society * Caving in the United Kingdom References External linksClub Website Clubs and societies of the U ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steinbrücken Cave
Steinbrücken Cave (german: Steinbrückenhöhle, "Stone bridge cave", no. 1623/204 in the Austrian cave register) was discovered by the Cambridge University Caving Club on the Loser Plateau in 1999. It is part of the large Schwarzmooskogel cave system (german: Schwarzmooskogelhöhlensystem), and is named after a nearby natural arch. The arch is in fact a former entrance to Traungold Cave (1623/231e) which has been developed into a convenient bivouac shelter for cave explorers. It is the List of longest caves, 17th longest cave system in the world. Layout As of 2013, the cave has six entrances, has passages of in length and a depth of . There are over 300 question marks (unexplored leads) of varying quality in the cave. The position of the first entrance is Alt 1812.40, . The originally discovered entrance A is primarily used as a route to the deepest part of the cave, "Razor Dance", a narrow rift of over extent. 32 pitches and climbs are required to reach the terminal sump. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Austria
The following article shows a list of caves in Austria. The list also includes ice caves and tourist former salt caves (''Salzwelten''). Overview The main concentration of Austrian caves (German: ''Höhle'') is in the Northern Limestone Alps, a mountain range of the Eastern Alps. Many of them are located in the geographical region of Salzkammergut and in the Totes Gebirge. Caves The caves are listed by alphabetical order and there are shown the main tourist caves and other notable (ex.: archaeological or paleontological) underground voids. In the "length" section is shown, between parentheses, the cave's trail as a show cave (SC). See also *List of caves * Simplified list for Austria * Speleology * Underground mines in Austria Notes References External links Schauhoehlen.at - Official Austrian showcaves portal [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Caves
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
