Lokomotive 85007 22
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]   |
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Grade (climbing)
In rock climbing, mountaineering, and other climbing disciplines, climbers give a grade to a climbing route or boulder problem, intended to describe concisely the difficulty and danger of climbing it. Different types of climbing (such as sport climbing, bouldering or ice climbing) each have their own grading systems, and many nationalities developed their own, distinctive grading systems. There are a number of factors that contribute to the difficulty of a climb, including the technical difficulty of the moves, the strength, stamina and level of commitment required, and the difficulty of protecting the climber. Different grading systems consider these factors in different ways, so no two grading systems have an exact one-to-one correspondence. Climbing grades are inherently subjective.Reynolds Sagar, Heather, 2007, ''Climbing your best: training to maximize your performance'', Stackpole Books, UK, 9. They may be the opinion of one or a few climbers, often the first ascensioni ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rock Formations Of Saxon Switzerland
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an isl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Teufelsturm (Saxon Switzerland)
The Teufelsturm (also ''Butterweckfels'' or ''Mittagstein'') is a prominent rock tower and climbing rock formed of Elbe Sandstone, about forty metres high in Saxon Switzerland in northeastern Germany. It is located east of the River Elbe on the upper edge of the valley between Schmilka and Bad Schandau in the Schrammsteinen. The Teufelsturm is also referred to as the "Symbol of Saxon Climbing". Origin of the name The oldest name for the peak is probably ''Butterweck'' ("Bread and butter") or ''Butterweckfels'', because the summit bears a certain resemblance to a bread roll when seen from a distance, such as from the other bank of the Elbe. The name ''Teufelsturm'' was already being used by Wilhelm Leberecht Götzinger in his descriptions of Saxon Switzerland, where he mentioned it as a sundial by the farmers on the plateaux around Schöna and Reinhardtsdorf. The shadow thrown by the Teufelsturm on the rock face behind it - when seen from the direction of Reinhardtsdorf-Schön ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Barbarine
The Barbarine is the best-known free-standing rock formation in the German part of the Elbe Sandstone Mountains. It is a rock pinnacle, high, and is the symbol of Saxon Switzerland. It was first climbed on 19 September 1905. Location The Barbarine belongs to the Pfaffenstein massif near the village of Pfaffendorf in the borough of Königstein. Development for sport climbing An ascent by the climber, Felix Wendschuh, on 9 September 1905 was the first documented attempt to climb the Barbarine. He climbed up to a point underneath the summit block, at least to the end of the crevice. The story that Keiler, the publican in Pfaffenstein, had forced him to turn around under threat, should probably be discounted. Keiler was a climber himself and would have had nothing against a climb, especially as those who first climbed it later left documentary evidence with him in the pub. On 19 September 1905 the Dresden climber, Rudolf Fehrmann, and the American, Oliver Perry-Smith, succeede ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Climbing Peak
A climbing peak (german: Klettergipfel) may refer to a mountain or hill peak or a rock formation that has to be ascended by climbing. The term is common in Germany where it is specifically used of free-standing rock formations in the climbing regions of Saxon Switzerland, Zittau Mountains and other nearby ranges in the German Central Uplands that can only be summitted via climbing routes of at least grade I on the UIAA scale or by jumping from nearby rocks or massifs. As a general rule, they must have a topographic prominence of at least 10 metres to qualify. In Saxon Switzerland the Saxon Climbing Regulations do not require any minimum height, but define climbing peaks as Another requirement is its recognition by the responsible sub-committee of the Saxon Climbers' Federation (SBB) and the responsible conservation authorities. For hikers these authorized summits may often be recognised by the presence of a summit register and abseiling anchor points. In other climbing ar ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Climbing Route
A climbing route is a path by which a climber reaches the top of a mountain, rock, or ice wall. Routes can vary dramatically in difficulty and grade; once committed to that ascent, it can sometimes be difficult to stop or return. Choice of route can be critically important. Guidebooks, if available, are helpful in providing detailed diagrams and photographs of routes. In the earliest days of hillwalking and mountaineering, climbers got to the top by whatever means got them there. Little information about how they did it is available. During the 19th century, as explorers of the Alps tried ever harder summits, it became clear that choosing an eastern face over a southwestern ridge could spell the difference between success or failure. One example was the first ascent of the Matterhorn, which had been repeatedly and unsuccessfully attempted via the southern side. The strata there tended to slope down and away while the rocks of the northeastern ridge (the one closest to Ze ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Fracture (geology)
A fracture is any separation in a geologic formation, such as a Joint (geology), joint or a Fault (geology), fault that divides the Rock (geology), rock into two or more pieces. A fracture will sometimes form a deep fissure or crevice in the rock. Fractures are commonly caused by Stress (physics), stress exceeding the rock strength, causing the rock to lose cohesion along its weakest plane. Fractures can provide Permeability (fluid), permeability for fluid movement, such as water or hydrocarbons. Highly fractured rocks can make good aquifers or Oil reservoir, hydrocarbon reservoirs, since they may possess both significant Permeability (fluid), permeability and fracture porosity. Brittle deformation Fractures are forms of brittle deformation. There are two types of primary brittle deformation processes. Tensile fracturing results in ''joints''. ''Shear fractures'' are the first initial breaks resulting from shear forces exceeding the cohesive strength in that plane. After those ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Climbing Rock
A climbing rock (german: Kletterfelsen; regionally also ''Kletterfels'' or '' Klettergipfel'') is a term used especially in Germany for an individual rock formation, rock face or rock group on which climbing is permitted. Designated climbing rocks are listed in climbing guidebooks and are usually incorporated and marked within the climbing areas of the alpine clubs. The concept is mainly relevant to climbing outside or on the fringes of the Alps. Special climbing regulations normally apply to climbing rocks, such as those for Saxon Switzerland, and there are usually restrictions to take account of conservation laws and requirements. {{webarchive, url=https://web.archive.org/web/20120424231154/http://www.alpenverein-bw.de/klettern/leitbild.html , date=2012-04-24 Exa ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chimney (climbing)
__NOTOC__ This glossary of climbing terms is a list of definitions of terms and jargon related to rock climbing and mountaineering. The specific terms used can vary considerably between different English-speaking countries; many of the phrases described here are particular to the United States and the United Kingdom. A B Completing the climb upon one's first attempt ever. Often confused with 'flashing' which is the first attempt of the day. There is a second opportunity for a climber to 'blitz' a wall after 12 months. C D E ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rock Face
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also featur ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |