|
Å krlatica
Škrlatica, historically also known as Suhi plaz ("Dry Avalanche"), 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). The mountain's name is the feminine adjectival form of the Slovene word ', a cognate of "scarlet," referring to the dramatic reddish-purple shade of the steep northwestern rockface in the reddish light of sunset. The alternate name ''Suhi plaz'' refers to a scree below Mount Spodnji Rokav. The first recorded ascent of Škrlatica was made from the southern side on 24 August 1880 by 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 refle ..., accompa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 ''Alpe Iulia'', and also attested as ''Alpes Juliana'' 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 Julian clan, perhaps due to a road built by Julius Caesar and completed by Aug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovenia
Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, and the Adriatic Sea to the southwest. Slovenia is mostly mountainous and forested, covers , and has a population of 2.1 million (2,108,708 people). Slovenes constitute over 80% of the country's population. Slovene, a South Slavic language, is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. A sub-mediterranean climate reaches to the northern extensions of the Dinaric Alps that traverse the country in a northwest–southeast direction. The Julian Alps in the northwest have an alpine climate. Toward the northeastern Pannonian Basin, a continental climate is more pronounced. Ljubljana, the capital and largest city of Slovenia, is geogr ... [...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] |
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'' , 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 ... [...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] |
Slovene Language
Slovene ( or ), or alternatively Slovenian (; or ), is a South Slavic languages, South Slavic language, a sub-branch that is part of the Balto-Slavic languages, Balto-Slavic branch of the Indo-European languages, Indo-European language family. It is spoken by about 2.5 million speakers worldwide (excluding speakers of Kajkavian), mainly ethnic Slovenes, the majority of whom live in Slovenia, where it is the sole official language. As Slovenia is part of the European Union, Slovene is also one of its 24 Languages of the European Union, official and working languages. Standard Slovene Standard Slovene is the national standard language that was formed in the 18th and 19th century, based on Upper Carniolan dialect group, Upper and Lower Carniolan dialect groups, more specifically on language of Ljubljana and its adjacent areas. The Lower Carniolan dialect group was the dialect used in the 16th century by Primož Trubar for his writings, while he also used Slovene as spoken in Lju ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cognate
In historical linguistics, cognates or lexical cognates are sets of words in different languages that have been inherited in direct descent from an etymology, etymological ancestor in a proto-language, common parent language. Because language change can have radical effects on both the sound and the meaning of a word, cognates may not be obvious, and often it takes rigorous study of historical sources and the application of the comparative method to establish whether lexemes are cognate or not. Cognates are distinguished from Loanword, loanwords, where a word has been borrowed from another language. The term ''cognate'' derives from the Latin noun '':wikt:cognatus, cognatus blood relative'. Characteristics Cognates need not have the same meaning, which semantic drift, may have changed as the languages developed independently. For example English language, English ''wikt:starve#English, starve'' and Dutch language, Dutch ''wikt:sterven#Dutch, sterven'' 'to die' or German languag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
