1.
Slovene language
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Slovene or Slovenian belongs to the group of South Slavic languages. It is spoken by approximately 2.5 million speakers worldwide and it is the first language of about 2.1 million Slovenian people and is one of the 24 official and working languages of the European Union. Standard Slovene is the standard language that was formed in the 18th century, mostly based on Upper and Lower Carniolan dialect groups. For example, the Resian and Torre dialects in the Italian Province of Udine differ most from other Slovene dialects, the distinctive characteristics of Slovene are dual grammatical number, two accentual norms, and abundant inflection. Although Slovene is basically an SVO language, word order is very flexible, Slovene has a T-V distinction, second-person plural forms are used for individuals as a sign of respect. Slovene and Slovak are the two modern Slavic languages whose names for themselves literally mean Slavic. Slovene is an Indo-European language belonging to the Western subgroup of the South Slavic branch of the Slavic languages, furthermore, Slovene shares certain linguistic characteristics with all South Slavic languages, including those of the Eastern subgroup, such as Bulgarian. The Slovene language also has commonalities with the West Slavic languages. Like all Slavic languages, Slovene traces its roots to the same group of languages that produced Old Church Slavonic. The earliest known examples of a distinct, written Slovene dialect are from the Freising Manuscripts, the consensus estimate of their date of origin is between 972 and 1093. These religious writings are among the oldest surviving manuscripts in any Slavic language and this linguistic border remained almost unchanged until the late 19th century, when a second process of Germanization took place, mostly in Carinthia. Between the 9th and 12th century, proto-Slovene spread into northern Istria, during most of the Middle Ages, Slovene was a vernacular language of the peasantry, although it was also spoken in most of the towns on Slovene territory, together with German or Italian. Although during this time, German emerged as the language of the nobility, Slovene had some role in the courtly life of the Carinthian, Carniolan and Styrian nobility. This is proved by the survival of certain ritual formulas in Slovene, the words Buge waz primi, gralva Venus. The first printed Slovene words, stara pravda, appeared in 1515 in Vienna in a poem of the German mercenaries who suppressed the Slovene peasant revolt. Standard Slovene emerged in the half of the 16th century, thanks to the works of Slovene Lutheran authors. During this period, German had a influence on Slovene. Many Slovene scientists before the 1920s also wrote in languages, mostly German
2.
Karst
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Karst topography is a landscape formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves and 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, the English word karst was borrowed from German Karst in the late 19th century. The German word came into use before the 19th century, according to the prevalent interpretation, the term is derived from the German name for the Karst region, a limestone plateau above the city of Trieste in the northern Adriatic. Scholars disagree, however, on whether the German word was borrowed from Slovene, the Slovene common noun kras was first attested in the 18th century, and the adjective form kraški in the 16th century. The Slovene words arose through metathesis from the reconstructed form *korsъ, ultimately, the word is of Mediterranean origin, believed to derive from some Romanized Illyrian base. It has been suggested that the word may derive from the Proto-Indo-European root karra- rock, the name may also be connected to the oronym Karsádios oros cited by Ptolemy, and perhaps also to Latin Carusardius. The development of karst occurs whenever acidic water starts to break down the surface of bedrock near its cracks, as the bedrock continues to degrade, its cracks tend to get bigger. As time goes on, these fractures will become wider, if this underground drainage system does form, it will speed up the development of karst formations there because more water will be able to flow through the region, giving it more erosive power. The carbonic acid that causes karstic features is formed as rain passes through the atmosphere picking up carbon dioxide, once the rain reaches the ground, it may pass through soil that can provide much more CO2 to form a weak carbonic acid solution, which dissolves calcium carbonate. The oxidation of sulfides leading to the formation of acid can also be one of the corrosion factors in karst formation. As oxygen -rich surface waters seep into deep anoxic karst systems, they bring oxygen, sulfuric acid then reacts with calcium carbonate, causing increased erosion within the limestone formation. This chain of reactions is, This reaction chain forms gypsum, the karstification of a landscape may result in a variety of large- or small-scale features both on the surface and beneath. On exposed surfaces, small features may include solution flutes, runnels, limestone pavement, medium-sized surface features may include sinkholes or cenotes, vertical shafts, foibe, disappearing streams, and reappearing springs. Large-scale features may include limestone pavements, poljes, and karst valleys, mature karst landscapes, where more bedrock has been removed than remains, may result in karst towers, or haystack/eggbox landscapes. Beneath the surface, complex underground systems and extensive caves. Some of the most dramatic of these formations can be seen in Thailands Phangnga Bay, calcium carbonate dissolved into water may precipitate out where the water discharges some of its dissolved carbon dioxide. Rivers which emerge from springs may produce tufa terraces, consisting of layers of calcite deposited over extended periods of time, in caves, a variety of features collectively called speleothems are formed by deposition of calcium carbonate and other dissolved minerals
3.
Kanin Mountains
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The Kanin Mountains or the Canin Mountains, mostly simply Kanin or Canin, are a mountain range in the Western Julian Alps, on the border of Slovenia and Italy. Their highest summit, Big Mount Kanin is 2,587 m above sea level and they separate the upper Soča Valley in Slovenia from the Resia Valley in Italy. On the Slovenian side of the range, which is part of the Municipality of Bovec, lies a major ski resort. Among a number of shafts, Vrtoglavica Cave holds the record for having the deepest single vertical drop of any cave on earth, 2½ hrs From D Postaja, a challenging marked route. 5 hrs From B Postaja, a challenging marked route. 6¼ hrs From the Sella Nevea pass, climbing the via ferrata Rosalba Grasselli, 4¾ hrs From the Sella Nevea pass, climbing the via ferrata Divisione Julia, a very challenging marked route. Kanin-Sella Nevea Ski Resort Media related to Kanin at Wikimedia Commons Kanin on Geopedia Kanin Ski Resort Visoki Kanin on Hribi. net, Routes and Photos
4.
Julian Alps
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They are named after Julius Caesar, who founded the municipium of Cividale del Friuli at the foot of the mountains. A large part of the Julian Alps is included in Triglav National Park, the second highest peak of the range, the 2,775 m high Jôf di Montasio, lies in Italy. The Julian Alps cover an estimated 4,400 km2 and they are located between the Sava Valley and Canale Valley. They are divided into the Eastern and Western Julian Alps, there are many peaks in the Eastern Julian Alps over 2,000 m high, and they are mainly parts of ridges. The most prominent peaks are visible by their height and size, there are high plains on the eastern border like Pokljuka, Mežakla and Jelovica. Only the Kanin group lies in part in Slovenia, the main peaks by height are, Jôf di Montasio Jof Fuart High Mount Kanin Important passes of the Julian Alps are, The Vršič Pass,1,611 m, links the Sava and Soča valleys. It is the highest mountain pass in Slovenia
5.
Slovenia
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Slovenia, officially the Republic of Slovenia, is a nation state in southern Central Europe, located at the crossroads of main European cultural and trade routes. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the south and southeast, and it covers 20,273 square kilometers and has a population of 2.06 million. It is a republic and a member of the United Nations, European Union. The capital and largest city is Ljubljana, additionally, the Dinaric Alps and the Pannonian Plain meet on the territory of Slovenia. The country, marked by a significant biological diversity, is one of the most water-rich in Europe, with a river network, a rich aquifer system. Over half of the territory is covered by forest, the human settlement of Slovenia is dispersed and uneven. Slovenia has historically been the crossroads of South Slavic, Germanic, Romance, although the population is not homogeneous, the majority is Slovene. South Slavic language Slovene is the language throughout the country. Slovenia is a largely secularized country, but its culture and identity have been influenced by Catholicism as well as Lutheranism. The economy of Slovenia is small, open, and export-oriented and has strongly influenced by international conditions. It has been hurt by the Eurozone crisis, started in the late 2000s. The main economic field is services, followed by industry and construction, Historically, the current territory of Slovenia was part of many different state formations, including the Roman Empire and the Holy Roman Empire, followed by the Habsburg Monarchy. In October 1918, the Slovenes exercised self-determination for the first time by co-founding the State of Slovenes, Croats, in December 1918, they merged with the Kingdom of Serbia into the Kingdom of Serbs, Croats and Slovenes. During World War II, Slovenia was occupied and annexed by Germany, Italy, and Hungary, with a tiny area transferred to the Independent State of Croatia, in June 1991, after the introduction of multi-party representative democracy, Slovenia split from Yugoslavia and became an independent country. Present-day Slovenia has been inhabited since prehistoric times, and there is evidence of habitation from around 250,000 years ago. A pierced cave bear bone, dating from 43100 ±700 BP, in the 1920s and 1930s, artifacts belonging to the Cro-Magnon such as pierced bones, bone points, and needle were found by archaeologist Srečko Brodar in Potok Cave. It shows that wooden wheels appeared almost simultaneously in Mesopotamia and Europe, in the transition period between the Bronze age to the Iron age, the Urnfield culture flourished. Archaeological remains dating from the Hallstatt period have been found, particularly in southeastern Slovenia, among them a number of situlas in Novo Mesto, in the Iron Age, present-day Slovenia was inhabited by Illyrian and Celtic tribes until the 1st century BC
6.
Italy
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Italy, officially the Italian Republic, is a unitary parliamentary republic in Europe. Located in the heart of the Mediterranean Sea, Italy shares open land borders with France, Switzerland, Austria, Slovenia, San Marino, Italy covers an area of 301,338 km2 and has a largely temperate seasonal climate and Mediterranean climate. Due to its shape, it is referred to in Italy as lo Stivale. With 61 million inhabitants, it is the fourth most populous EU member state, the Italic tribe known as the Latins formed the Roman Kingdom, which eventually became a republic that conquered and assimilated other nearby civilisations. The legacy of the Roman Empire is widespread and can be observed in the distribution of civilian law, republican governments, Christianity. The Renaissance began in Italy and spread to the rest of Europe, bringing a renewed interest in humanism, science, exploration, Italian culture flourished at this time, producing famous scholars, artists and polymaths such as Leonardo da Vinci, Galileo, Michelangelo and Machiavelli. The weakened sovereigns soon fell victim to conquest by European powers such as France, Spain and Austria. Despite being one of the victors in World War I, Italy entered a period of economic crisis and social turmoil. The subsequent participation in World War II on the Axis side ended in defeat, economic destruction. Today, Italy has the third largest economy in the Eurozone and it has a very high level of human development and is ranked sixth in the world for life expectancy. The country plays a prominent role in regional and global economic, military, cultural and diplomatic affairs, as a reflection of its cultural wealth, Italy is home to 51 World Heritage Sites, the most in the world, and is the fifth most visited country. The assumptions on the etymology of the name Italia are very numerous, according to one of the more common explanations, the term Italia, from Latin, Italia, was borrowed through Greek from the Oscan Víteliú, meaning land of young cattle. The bull was a symbol of the southern Italic tribes and was often depicted goring the Roman wolf as a defiant symbol of free Italy during the Social War. Greek historian Dionysius of Halicarnassus states this account together with the legend that Italy was named after Italus, mentioned also by Aristotle and Thucydides. The name Italia originally applied only to a part of what is now Southern Italy – according to Antiochus of Syracuse, but by his time Oenotria and Italy had become synonymous, and the name also applied to most of Lucania as well. The Greeks gradually came to apply the name Italia to a larger region, excavations throughout Italy revealed a Neanderthal presence dating back to the Palaeolithic period, some 200,000 years ago, modern Humans arrived about 40,000 years ago. Other ancient Italian peoples of undetermined language families but of possible origins include the Rhaetian people and Cammuni. Also the Phoenicians established colonies on the coasts of Sardinia and Sicily, the Roman legacy has deeply influenced the Western civilisation, shaping most of the modern world
7.
Pitch (ascent/descent)
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In rock climbing and ice climbing, a pitch is a steep section of a route that requires a rope between two belays, as part of a climbing system. In free climbing, pitch refers to classification by climbers of the difficulty of ascent on certain climbing routes, in advanced climbing or mountaineering, another definition of pitch is not restricted by the length of the rope. On easier terrain or when moving quickly, the length of a pitch can be extended by means of simul climbing, effectively combining several pitches together by means of a running belay. Speed climbers will often state that they completed a route with a reduced number of pitches. This definition is used loosely, since the length of a pitch is limited by the nature of the terrain. Comparative The term pitch is used by cavers to refer to a very steep or vertical section in a cave that needs ladders or single rope technique to descend and ascend. As caving rope lengths are not standardized, the length of a pitch is equal to that of the drop. The deepest underground pitch is 603 m in Vrtiglavica Cave in the Julian Alps, in some cases, cavers may choose to split one drop into two or more distinct pitches. However in most cases a single rope or ladder is used for the drop, so in practical usage pitch has become synonymous with the terms drop. While a pitch refers to a drop that can be descended, if not free-climbable, avens can be ascended by means of a bolt climb, where a caver places an ascending series of bolts in the walls and gradually ascends to the top. A rope can then be rigged to the bottom allowing following cavers to pass the obstacle, some avens have been tackled by lifting ropes or ladders using long poles. Narrow avens can be climbed by pushing against opposite walls, pit cave Grade, a subjective numerical code for athletic difficulty. The worlds deepest pitches, by Bob Gulden Caves with the deepest drop, by Jochen Duckeck
8.
Quaternary glaciation
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During this period, ice sheets expanded, notably from out of Antarctica and Greenland, and fluctuating ice sheets occurred elsewhere. It affected oceans, flooding, and biological communities, the ice sheets themselves, by raising the albedo, affect a major feedback on climate cooling. The Quaternary glaciation was the first ice age to be demonstrated in geology and this was done over the 1700s and 1800s CE. Over the last century, extensive field observations have provided evidence that continental glaciers covered large parts of Europe, North America, even before the theory of worldwide glaciation was generally accepted, many observers recognized that more than a single advance and retreat of the ice had occurred. Since then other, earlier ice ages have been identified, the Quaternary glaciation is the last of five known glaciations during Earths history. The other four are the Huronian glaciation, Cryogenian, Andean-Saharan glaciation, over the past 740,000 years there have been eight glacial cycles. The entire Quaternary Period, starting 2.58 Ma, is referred to as an ice age because at least one permanent large ice sheet—the Antarctic ice sheet—has existed continuously, there is uncertainty over how much of Greenland was covered by ice during the previous and earlier interglacials. During the colder episodes—referred to as glacial ice sheets at least 4 km thick at their maximum also existed in Europe, North America. The shorter and warmer intervals between glacials are referred to as interglacials, currently, Earth is in an interglacial period, which marked the beginning of the Holocene epoch. The current interglacial began between 10,000 and 15,000 years ago, which caused the ice sheets from the last glacial period to begin to disappear. Remnants of these last glaciers, now occupying about 10% of the land surface, still exist in Greenland, Antarctica. During the glacial periods, the present hydrologic system was completely interrupted throughout large areas of the world and was modified in others. Due to the volume of ice on land, sea level was approximately 120 meters lower than present, extensive evidence now shows that a number of periods of growth and retreat of continental glaciers occurred during the ice age, called glacials and interglacials. The interglacial periods of climate are represented by buried soil profiles, peat beds. No completely satisfactory theory has been proposed to account for Earths history of glaciation, the cause of glaciation may be related to several simultaneous factors, such as astronomical cycles, atmospheric composition, plate tectonics, and ocean currents. The role of Earths orbital changes in controlling climate was first advanced by James Croll in the late 19th century, later, Milutin Milanković, a Serbian geophysicist, elaborated on the theory and calculated these irregularities in Earths orbit could cause the climatic cycles known as Milankovitch cycles. They are the result of the behavior of several types of cyclical changes in Earths orbital properties. Changes in the eccentricity of Earth occur on a cycle of about 100,000 years
