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Razor (mountain)
Razor () is a pyramidal mountain in the Julian Alps and the sixth-highest mountain in Slovenia. First ascended by Otto Sendtner in 1842, it is now frequently ascended, with numerous mountain huts available for climbers. Location and description Razor is part of the Julian Alps in Slovenia, and is bordered by the Luknja and Vršič passes to the east and west, and the Krnica and Trenta valleys to the north and south. Together with its neighbouring mountain Prisojnik, it serves to connect Triglav and Jalovec. It is included in Triglav National Park and is administratively part of Kranjska Gora. The mountain is located in a limestone karst region, with the Križ Plateau (''Kriški podi'') below it being a typical example. The area has been heavily shaped by erosion, caused by glaciation, rivers, and precipitation; as a result, it has many caves, sinkholes, and limestone pavements. Climate Razor is snow-covered from November to early June. Ascent Razor was first ascended ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prisojnik
Prisojnik or Prisank is a mountain of the Julian Alps in Slovenia. Its summit is 2,547m above sea level. It is located above the Vršič Pass The Vršič Pass (; sl, prelaz Vršič, it, passo della Moistrocca, german: Werschetzpass), with an elevation of , is a high mountain pass across the Julian Alps in northwestern Slovenia. It is the highest pass in Slovenia, as well as the high ..., from where most climbs of the mountain start. References External links Prisojnik on hribi.net Mountains of the Julian Alps Two-thousanders of Slovenia {{Slovenia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triglav
Triglav (; german: Terglau; it, Tricorno), with an elevation of , is the highest mountain in Slovenia and the highest peak of the Julian Alps. The mountain is the pre-eminent symbol of the Slovene nation. It is the centrepiece of Triglav National Park, Slovenia's only national park. Triglav was also the highest peak in Yugoslavia before Slovenia's independence in 1991. Name Various names have been used for the mountain through history. An old map from 1567 named it ''Ocra mons'', whereas Johann Weikhard von Valvasor named it ''Krma'' in the second half of the 17th century. According to the German mountaineer and professor Adolf Gstirner, the name ''Triglav'' first appeared in written sources as ''Terglau'' in 1452, but the original source has been lost. The next known occurrence of ''Terglau'' is cited by Gstirner and is from a court description of the border in 1573. Early forms of the name ''Triglav'' also include ''Terglau'' in 1612, ''Terglou'' in 1664 and ''Terklou'' arou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julius Kugy
Julius Kugy (19 July 1858 – 5 February 1944) was a mountaineer, writer, botanist, humanist, lawyer and officer of Slovenian descent. He wrote mostly in German. He is renowned for his travelogues from opening up the Julian Alps, in which he reflected on the relationship between man, nature, and culture. He opposed competing nationalist ideologies in the Alpe-Adria region, insisting on the need of peaceful co-existence among Slovene, Italian and German peoples. Biography Julius Kugy was born to Slovenian family in Gorizia, then part of the Austrian Empire (now in Italy). His father Paul was a farmer from Lind (''Lipa'') near Arnoldstein in the Carinthian Gail Valley. His mother Giulia was the daughter of the Slovene poet Janez Vesel. The surname ''Kugy'' has the same origin as the surnames ''Kugi'', ''Kogoj'', and ''Kogej''. Kugy was educated in a multi-lingual environment: from an early age he was fluent in three of the four languages of his native Gorizia and Gradisca region: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Technical Climb
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Via Ferrata
A via ferrata (Italian for "iron path", plural ''vie ferrate'' or in English ''via ferratas'') is a protected climbing route found in the Alps and certain other locations. The term "via ferrata" is used in most countries and languages except notably in German-speaking regions, which use ''Klettersteig''—"climbing path" (plural ''Klettersteige''). Infrastructure A via ferrata is a climbing route that employs steel cables, rungs or ladders, fixed to the rock to which the climbers affix a harness with two leashes, which allows the climbers to secure themselves to the metal fixture and limit any fall. The cable and other fixtures, such as iron rungs (stemples), pegs, carved steps, and ladders and bridges, provide both footings and handholds, as well. This allows climbing on otherwise dangerous routes without the risks of unprotected scrambling and climbing or the need for technical climbing equipment. They expand the opportunities for accessing difficult peaks as an alternative ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weather Underground (weather Service)
Weather Underground is a commercial weather service providing real-time weather information over the Internet. Weather Underground provides weather reports for most major cities around the world on its Web site, as well as local weather reports for newspapers and third-party sites. Its information comes from the National Weather Service (NWS), and over 250,000 personal weather stations (PWS). The site is available in many languages, and customers can access an ad-free version of the site with additional features for an annual fee. Weather Underground is owned by The Weather Company, a subsidiary of IBM. History The company is based in San Francisco, California and was founded in 1995 as an offshoot of the University of Michigan Internet weather database. The name is a reference to the 1960s radical left-wing militant organization the Weather Underground, which also originated at the University of Michigan. Jeff Masters, a doctoral candidate in meteorology at the Universit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Pavement
A limestone pavement is a natural karst landform consisting of a flat, incised surface of exposed limestone that resembles an artificial pavement. The term is mainly used in the UK and Ireland, where many of these landforms have developed distinctive surface patterning resembling paving blocks. Similar landforms in other parts of the world are known as alvars. Formation of a limestone pavement Conditions for limestone pavements are created when an advancing glacier scrapes away overburden and exposes horizontally bedded limestone, with subsequent glacial retreat leaving behind a flat, bare surface. Limestone is slightly soluble in water and especially in acid rain, so corrosive drainage along joints and cracks in the limestone can produce slabs called ''clints'' isolated by deep fissures called ''grikes'' or ''grykes'' (terms derived from a northern English dialect). If the grykes are fairly straight and the clints are uniform in size, the resemblance to man-made paving stone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triglav National Park
Triglav National Park (TNP) ( sl, Triglavski narodni park) is the only national park in Slovenia. It was established in its modern form in 1981 and is located in the northwestern part of the country, respectively the southeastern part of the Alpine massif. Mount Triglav, the highest peak of the Julian Alps, stands almost in the middle of the national park. From it the valleys spread out radially, supplying water to two large river systems with their sources in the Julian Alps: the Soča and the Sava, flowing to the Adriatic and Black Sea, respectively. History The proposal for the protection of the Triglav Lakes Valley area was first put forward by the seismologist Albin Belar in 1906 or 1908. However, the proposal was not accepted, as there was no legal base for it and the then valid laws prohibited any restriction of pasture. The strategic basis for the protection of the area, titled ''The Memorandum'' (), and which explicitly mentioned the proposal of Belar, was submitted to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jalovec (mountain)
Mount Jalovec (; it, Monte Gialuz) is a mountain in the Julian Alps. With an elevation of 2,645 m, it is the sixth-highest peak in Slovenia. It stands between the Tamar, Koritnica, and Trenta Alpine valleys. Nearby peaks include Mangart to the west, Travnik and Mojstrovka to the east, and Ponce to the north. The Log Cliff ( sl, Loška stena, it, Parete di Bretto) stands immediately southwest of Mount Jalovec. Name Mount Jalovec was attested in written sources as early as 1763–87 as ''Jellauz'' and ''Jelauz''. The name is derived from the Slovene adjective ''jalov'' 'barren, infertile', referring to the lack of vegetation on the slopes of the mountain. See also * List of mountains in Slovenia * Julian Alps The Julian Alps ( sl, Julijske Alpe, it, Alpi Giulie, , ) are a mountain range of the Southern Limestone Alps that stretch from northeastern Italy to Slovenia, where they rise to 2,864 m at Mount Triglav, the highest peak in Slovenia. A large pa ... References E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trenta (valley)
The Trenta Valley () is a valley in the Julian Alps in the northern part of the traditional Gorizia region ( sl, Goriška) of Slovenia. Geography The source of the Soča River and the settlements of Soča, Lepena, and Trenta are located in the Trenta Valley. The Vršič Pass connects the valley with Upper Carniola to the east. The Soča flows generally southwest through the valley and then onwards to Bovec Bovec ( or ; , german: Flitsch, fur, Plèz) is a town in the Littoral region in northwestern Slovenia, close to the border with Italy. It is the central settlement of the Municipality of Bovec. Geography Bovec is located from the capital Ljublj .... Name The name ''Trenta'' is of Friulian origin and was borrowed into Slovene. The name developed from ''*Tridenta'', meaning 'three-tooth' or 'divided into three teeth'. This reflects the geography because the valley splits into the Soča and Zadnjica valleys, and the latter is soon split again by White Creek (''Beli Potok'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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