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Karlspitzen
The Karlspitzen is a twin-peaked mountain in the middle of the Kaisergebirge range of the Northern Limestone Alps in Austria. The two peaks are the northern ''Hintere Karlspitze'' (2,281 m) and the southern ''Vordere Karlspitze'' (2,263 m) with its summit cross; they are linked by a sharp, exposed, rocky arête. Seen from the south the Vordere Karlspitze is a huge and very prominent block of rock, whereas the Hintere Karlspitze is hidden behind other (lower) neighbouring mountains. Location The Karlspitzen peaks tower over the Ellmauer Tor saddle and Steinerne Rinne couloir to their east and so lie in the heart of the Wilder Kaiser mountains. To the east rise the rather lower summits of the Goinger Halt and Predigtstuhl, immediately to the north are the Fleischbank and Totenkirchl and, further west, separated by the Kopftörl arête, is the higher Ellmauer Halt. Thanks to its location the Karlspitzen have extensive views over both the Wilder Kaiser and also the neighbouring ...
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Ellmauer Tor
The Ellmauer Tor is a 2,000-metre high rock saddle in the middle of the Kaisergebirge in the Austrian state of Tyrol. It is the deepest saddle on the main ridge of the Wilder Kaiser between the ''Ostkaisers Ackerlspitze in the East Kaiser and the Ellmauer Halt in the Central Kaiser mountains. Because there is a well-used route across the Ellmauer Tor with its unique setting, it is often referred to as the "heart of the Kaiser". From the south, seen from the general direction of Ellmau or Going, it is the distinctive notch in the Kaisergebirge between the Karlspitzen and the Goinger Halt. Routes The Ellmauer Tor is the most important and most frequently used crossing in the Wilder Kaiser. On clear summer's days countless climbers walk through here. The most famous way leads from the north, from the Stripsenjochhaus through the ''Steinerne Rinne'' to the Ellmauer Tor. For this route Alpine experience, secure footing and no fear of heights are indispensable, even though it is wel ...
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Kaisergebirge
The Kaiser Mountains (german: Kaisergebirge, meaning ''Emperor Mountains'') are a mountain range in the Northern Limestone Alps and Eastern Alps. Its main ridges – are the Zahmer Kaiser and south of it the Wilder Kaiser. The mountains are situated in the Austrian province of Tyrol between the town of Kufstein and the town of St. Johann in Tirol. The Kaiser Mountains offer some of the loveliest scenery in all the Northern Limestone Alps. Reynolds, Kev (2005). ''Walking in the Alps'', 2nd ed., Cicerone, Singapore, p. 430, . Divisions The Kaiser Mountains are divided into the Wilder Kaiser or Wild Kaiser chain of mountains, formed predominantly of bare limestone rock, and the Zahmer Kaiser ("Tame Kaiser"), whose southern side is mainly covered by mountain pine. These two mountain ridges are linked by the 1,580-metre-high Stripsenjoch pass, but are separated in the west by the valley of Kaisertal and in the east by the Kaiserbach valley. In total the Kaiser extends for abo ...
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Double Peak
A double summit, double peak, twin summit, or twin peak refers to a mountain or hill that has two summits, separated by a col or saddle. One well-known double summit is Austria’s highest mountain, the Großglockner, where the main summit of the Großglockner is separated from that of the Kleinglockner by the Glocknerscharte col in the area of a geological fault. Other double summits have resulted from geological folding. For example, on Mont Withrow in British Columbia, resistant sandstones form the limbs of the double summit, whilst the softer rock in the core of the fold was eroded.{{cite web , url=http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , title=Mt. Withrow syncline , archive-url=https://web.archive.org/web/20060404185911/http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , archive-date=2006-04-04 , access-date=2009-05-12 Triple peaks occur more rarely; one example is the Rosengartenspitze in the Dolomites. The Illimani in Bolivia is an example of a rare quadruple summit. ...
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Twin-peaked
A double summit, double peak, twin summit, or twin peak refers to a mountain or hill that has two summits, separated by a col or saddle. One well-known double summit is Austria’s highest mountain, the Großglockner, where the main summit of the Großglockner is separated from that of the Kleinglockner by the Glocknerscharte col in the area of a geological fault. Other double summits have resulted from geological folding. For example, on Mont Withrow in British Columbia, resistant sandstones form the limbs of the double summit, whilst the softer rock in the core of the fold was eroded.{{cite web , url=http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , title=Mt. Withrow syncline , archive-url=https://web.archive.org/web/20060404185911/http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , archive-date=2006-04-04 , access-date=2009-05-12 Triple peaks occur more rarely; one example is the Rosengartenspitze in the Dolomites. The Illimani in Bolivia is an example of a rare quadruple summit. ...
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Steinerne Rinne (Kaisergebirge)
The Predigtstuhl is a high mountain in the Wilder Kaiser range in the Northern Limestone Alps in Austria, east of Kufstein in the Tyrol. The mountain is one of the well-known climbing mountains in the Northern Limestone Alps. Among its most famous climbing routes are the Angermann Gully (''Angermannrinne'') (normal route at UIAA grade III via the Predigtstuhl wind gap), the striking North Rim (''Nordkante'') and the Botzong Chimney (''Botzong-Kamin''). The start point for these routes is the Stripsenjochhaus mountain hut belonging to the Austrian Alpine Club (ÖAV). Together with the Hinterer Goinger Halt, Karlspitzen, Fleischbank and Christaturm the peak forms the rim of the Steinerne Rinne, a huge couloir and old glacial cirque, that runs southwards up to the crossing of the Ellmauer Tor The Ellmauer Tor is a 2,000-metre high rock saddle in the middle of the Kaisergebirge in the Austrian state of Tyrol. It is the deepest saddle on the main ridge of the Wilder Kaiser betwe ...
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Goinger Halt
The Goinger Halt is a mountain in the Kaisergebirge range in the Northern Limestone Alps in Austria. It has a double summit: a northern top to the rear, the ''Hintere Goinger Halt'' (2,192 metres), and a higher, southern top in front, the ''Vordere Goinger Halt'' (2,242 metres). The name "Halt" means something like Alpine meadow and refers therefore to the peak over the meadow areas, that belong to the parish of Going (c.f. Ellmauer Halt). Location The Goinger Halt climbs immediately east of the Ellmauer Tor from the cirque of the Steinerne Rinne and so lies in the central part of the Kaisergebirge. Opposite it to the west are the peaks of the Karlspitzen and the Fleischbank. To the north the Halt is preceded by the Predigtstuhl. The main crest of the mountain ridge runs away to the southwest, finally culminating in the Ackerlspitze and, to the northwest, steep rock faces plunge into the Griesner Cirque. Routes The Hintere Goinger Halt counts as one of the easiest and ther ...
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Predigtstuhl (Kaisergebirge)
The Predigtstuhl is a high mountain in the Wilder Kaiser range in the Northern Limestone Alps in Austria, east of Kufstein in the Tyrol. The mountain is one of the well-known climbing mountains in the Northern Limestone Alps. Among its most famous climbing routes are the Angermann Gully (''Angermannrinne'') (normal route at UIAA grade III via the Predigtstuhl wind gap), the striking North Rim (''Nordkante'') and the Botzong Chimney (''Botzong-Kamin''). The start point for these routes is the Stripsenjochhaus mountain hut belonging to the Austrian Alpine Club (ÖAV). Together with the Hinterer Goinger Halt, Karlspitzen, Fleischbank and Christaturm the peak forms the rim of the Steinerne Rinne, a huge couloir and old glacial cirque A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform ...
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Mountains Of Tyrol (state)
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains Of The Alps
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , and all of them exceeding in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion. The list of these most prominent mountains is continued down to 2500 m elevation at List of prominent mountains of the Alps (2500–2999 m) and down to 2000 m elevation on List of prominent mountains of the Alps (2000–2499 m). All such mountains are located in either France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these three lists include all 44 ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpi ...
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Climbing Grade
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 ascensi ...
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Schrofen
Schrofen, a German mountaineering term, is steep terrain, strewn with rocks and rock outcrops, that is laborious to cross, but whose rock ledges (''schrofen'') offer many good steps and hand holds. It is usually rocky terrain on which grass has established itself, but it can also refer to purely rocky slopes. ''Schrofen'' are found especially where the rock has broken off against its angle of dip. ''Schrofen'' differs from trackless terrain in that hands are needed in order to negotiate it. Often there are route markings that only indicate a rough direction.''So gehen Sie sicher im Schrofengelände''
("How to negotiate ''schrofen'' terrain safely") at www.alpin.de. Accessed on 31 Dec 2010 ''Schrofen'' terrain requires at least

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Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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