Å krlatica
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Å krlatica
Škrlatica, historically also known as Suhi plaz, is a mountain in the Slovenian Julian Alps. With its summit at 2,740m above sea level, it is the second-highest peak in Slovenia (after Triglav at 2,864m) and the third highest in the Julian Alps as a whole (after Triglav and Jôf di Montasio / Montaž at 2,754m). Despite its height, the mountain has a low prominence, as its peak is part of a long, curtain-like ridge. Name The name ''Škrlatica'' is a dialect development from *''Škriljatica'', derived from ''škril'' 'stone slab', referring to a mountain with many stone slabs. The name is unrelated to the Slovene color word ''škrlat'' 'scarlet'. The mountain's archaic name, ''Suhi plaz,'' pertains to an avalanche-prone scree Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. The term ''scree'' is ap ... b ...
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Slovenia
Slovenia, officially the Republic of Slovenia, is a country in Central Europe. It borders Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the south and southeast, and a short (46.6 km) coastline within the Adriatic Sea to the southwest, which is part of the Mediterranean Sea. Slovenia is mostly mountainous and forested, covers , and has a population of approximately 2.1 million people. Slovene language, Slovene is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. Ljubljana, the capital and List of cities and towns in Slovenia, largest city of Slovenia, is geographically situated near the centre of the country. Other larger urban centers are Maribor, Ptuj, Kranj, Celje, and Koper. Slovenia's territory has been part of many different states: the Byzantine Empire, the Carolingian Empire, the Holy Roman Empire, the Kingdom of Hungary, the Republic of Venice ...
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Julian Alps
The Julian Alps (, , , , ) are a mountain range of the Southern Limestone Alps that stretches from northeastern Italy to Slovenia, where they rise to 2,864 m at Mount Triglav, the highest peak in Slovenia. A large part of the Julian Alps is included in Triglav National Park. The second highest peak of the range, the 2,755 m high Jôf di Montasio, lies in Italy. The Julian Alps cover an estimated 4,400 km2 (of which 1,542 km2 lies in Italy). They are located between the Sava Valley and Canale Valley. They are divided into the Eastern and Western Julian Alps. Name The Julian Alps were known in antiquity as ''Alpes Iuliae'', and also attested as ''Alpes Julianae'' AD 670, ''Alpis Julia'' 734, and ''Alpes Iulias'' in 1090. Like the municipium of ''Forum Julii'' (now Cividale del Friuli) at the foot of the mountains, the range was named after Julius Caesar of the gens Julia, perhaps due to a road built by Julius Caesar and completed by Augustus. Eastern Julian A ...
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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 regi ...
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List Of Mountains Of The Alps (2500–2999 M)
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , all 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 France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these lists include all 44 List of Alpine peaks by prominence, ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 of the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to ...
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Triglav
Triglav (; ; ), 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, appearing on the Coat of arms of Slovenia, coat of arms and Flag of Slovenia, flag of Slovenia. It is the centrepiece of Triglav National Park, Slovenia's only national park. Triglav was also the highest peak in Socialist Federal Republic of Yugoslavia, Yugoslavia before Slovenia's independence in 1991. Name Various names have been used for the mountain through history. An old map from 1567 used the Latin name ''Ocra mons'', whereas Johann Weikhard von Valvasor called it ''Krma'' (the modern name of an Alpine valley in the vicinity) 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 b ...
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Topographic Prominence
In topography, prominence or relative height (also referred to as autonomous height, and shoulder drop in US English, and drop in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. The key col ("saddle") around the peak is a unique point on this contour line and the ''parent peak'' (if any) is some higher mountain, selected according to various criteria. Definitions The prominence of a peak is the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following manner: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''highest saddle (landform), saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prominence is the differ ...
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Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. The term ''scree'' is applied both to an unstable steep mountain slope composed of rock fragments and other debris, and to the mixture of rock fragments and debris itself. It is loosely synonymous with talus, material that accumulates at the base of a projecting mass of rock, or talus slope, a landform composed of talus. The term ''scree'' is sometimes used more broadly for any sheet of loose rock fragments mantling a slope, while ''talus'' is used more narrowly for material that accumulates at the base of a cliff or other rocky slope from which it has obviously eroded. Scree is formed by rockfall, which distinguishes it from colluvium. Colluvium is rock fragments or soil deposited by rainwash, sheetwash, or slow downhill creep, usually at the base of gentle ...
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Mountains Of The Julian Alps
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 above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ...
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