1.
Italian language
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By most measures, Italian, together with Sardinian, is the closest to Latin of the Romance languages. Italian is a language in Italy, Switzerland, San Marino, Vatican City. Italian is spoken by minorities in places such as France, Montenegro, Bosnia & Herzegovina, Crimea and Tunisia and by large expatriate communities in the Americas. Many speakers are native bilinguals of both standardized Italian and other regional languages, Italian is the fourth most studied language in the world. Italian is a major European language, being one of the languages of the Organisation for Security and Cooperation in Europe. It is the third most widely spoken first language in the European Union with 65 million native speakers, including Italian speakers in non-EU European countries and on other continents, the total number of speakers is around 85 million. Italian is the working language of the Holy See, serving as the lingua franca in the Roman Catholic hierarchy as well as the official language of the Sovereign Military Order of Malta. Italian is known as the language of music because of its use in musical terminology and its influence is also widespread in the arts and in the luxury goods market. Italian has been reported as the fourth or fifth most frequently taught foreign language in the world, Italian was adopted by the state after the Unification of Italy, having previously been a literary language based on Tuscan as spoken mostly by the upper class of Florentine society. Its development was influenced by other Italian languages and to some minor extent. Its vowels are the second-closest to Latin after Sardinian, unlike most other Romance languages, Italian retains Latins contrast between short and long consonants. As in most Romance languages, stress is distinctive, however, Italian as a language used in Italy and some surrounding regions has a longer history. What would come to be thought of as Italian was first formalized in the early 14th century through the works of Tuscan writer Dante Alighieri, written in his native Florentine. Dante is still credited with standardizing the Italian language, and thus the dialect of Florence became the basis for what would become the language of Italy. Italian was also one of the recognised languages in the Austro-Hungarian Empire. Italy has always had a dialect for each city, because the cities. Those dialects now have considerable variety, as Tuscan-derived Italian came to be used throughout Italy, features of local speech were naturally adopted, producing various versions of Regional Italian. Even in the case of Northern Italian languages, however, scholars are not to overstate the effects of outsiders on the natural indigenous developments of the languages
2.
German language
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German is a West Germanic language that is mainly spoken in Central Europe. It is the most widely spoken and official language in Germany, Austria, Switzerland, South Tyrol, the German-speaking Community of Belgium and it is also one of the three official languages of Luxembourg. Major languages which are most similar to German include other members of the West Germanic language branch, such as Afrikaans, Dutch, English, Luxembourgish and it is the second most widely spoken Germanic language, after English. One of the languages of the world, German is the first language of about 95 million people worldwide. The German speaking countries are ranked fifth in terms of publication of new books. German derives most of its vocabulary from the Germanic branch of the Indo-European language family, a portion of German words are derived from Latin and Greek, and fewer are borrowed from French and English. With slightly different standardized variants, German is a pluricentric language, like English, German is also notable for its broad spectrum of dialects, with many unique varieties existing in Europe and also other parts of the world. The history of the German language begins with the High German consonant shift during the migration period, when Martin Luther translated the Bible, he based his translation primarily on the standard bureaucratic language used in Saxony, also known as Meißner Deutsch. Copies of Luthers Bible featured a long list of glosses for each region that translated words which were unknown in the region into the regional dialect. Roman Catholics initially rejected Luthers translation, and tried to create their own Catholic standard of the German language – the difference in relation to Protestant German was minimal. It was not until the middle of the 18th century that a widely accepted standard was created, until about 1800, standard German was mainly a written language, in urban northern Germany, the local Low German dialects were spoken. Standard German, which was different, was often learned as a foreign language with uncertain pronunciation. Northern German pronunciation was considered the standard in prescriptive pronunciation guides though, however, German was the language of commerce and government in the Habsburg Empire, which encompassed a large area of Central and Eastern Europe. Until the mid-19th century, it was essentially the language of townspeople throughout most of the Empire and its use indicated that the speaker was a merchant or someone from an urban area, regardless of nationality. Some cities, such as Prague and Budapest, were gradually Germanized in the years after their incorporation into the Habsburg domain, others, such as Pozsony, were originally settled during the Habsburg period, and were primarily German at that time. Prague, Budapest and Bratislava as well as cities like Zagreb, the most comprehensive guide to the vocabulary of the German language is found within the Deutsches Wörterbuch. This dictionary was created by the Brothers Grimm and is composed of 16 parts which were issued between 1852 and 1860, in 1872, grammatical and orthographic rules first appeared in the Duden Handbook. In 1901, the 2nd Orthographical Conference ended with a standardization of the German language in its written form
3.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
4.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
5.
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 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
6.
Province of Belluno
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The Province of Belluno is a province in the Veneto region of Italy. Its capital is the city of Belluno and it has an area of 3,678 square kilometres and a total population of about 200,000. The province of Belluno is rather wide, and almost entirely occupied by mountain areas and it encompasses the natural and historical regions of Cadore, Feltrino, Alpago, Val di Zoldo, Agordino, Comelico and Ampezzano. The eastern part of the features the Dolomites, including the famous Tofane, Marmolada, Tre Cime di Lavaredo. The province is rich in water, with the presence of the wide Piave River, with its affluents Boite, the southern part is called Valbelluna, the widest and most populous valley of the province, which is bordered by the Venetian Prealps. The National Park of Belluno Dolomites is located in the province, the province of Bellunos climate is among the most severe in the Alps. It is mostly influenced by the continentally, provided by the Dolomites and it is similar to the eastern Tyrols climate. The summers are hot but not as hot as the valleys of the rivers Po, the hottest month’s average temperature is between 18 °C and 21 °C. This area, as most of the oriental Alps, is very wet, belluno’s precipitation average is above 1300 mm per year, snow is usual during all the winter months, and may occur even in March or November. Some years the winter may be due to the humidity, with averages around the freezing point. Main cities in area, Belluno, Feltre, Seren del Grappa. The midland’s valleys, between 700 m and 1500 m, which have a humid continental climate Dfb. This climate is severe in the extreme northern or southwestern regions of the province. Winter’s average temperature is between −7 °C and −5 °C in the North and Southwest during January, and between −5 °C and −3 °C around the central region. The coldest town, Santo Stefano di Cadore, at an elevation of only 900 meters, has temperature averages in January between −7 °C and −6 °C. Other towns of relatively low elevations have really low averages, which would be found only above 1700 meters in other Italians provinces, the snow season depends on the altitude. Between 700 and 1200 meters, from early November until the middle of March, the summer is usually wet and mild, but hotter than areas at the same altitude in the occidental valleys. In the lower lands temperature average around 16 °C or 17 °C, in higher lands average around 14 °C
7.
South Tyrol
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South Tyrol, also known by its alternative Italian name Alto Adige, is an autonomous province in northern Italy. It is one of the two provinces that make up the autonomous region of Trentino-Alto Adige/Südtirol. The province has an area of 7,400 square kilometres and its capital is the city of Bolzano. As of 2011, South Tyrol is among the wealthiest regions in Italy, South Tyrol is the term most commonly used in English for the province, and its usage reflects that it was created from a portion of the southern part of the historic County of Tyrol. German and Ladin speakers usually refer to the area as Südtirol, Alto Adige, one of the Italian names for the province, is also used in English. The term had been the name of political subdivisions along the Adige River in the time of Napoleon Bonaparte and it was reused as the Italian name of the current province after its post-World War I creation, and was a symbol of the subsequent forced Italianization of South Tyrol. The official name of the today in German is Autonome Provinz Bozen — Südtirol. German speakers usually refer to it not as a Provinz, provincial institutions are referred to using the prefix Landes-, such as Landesregierung and Landeshauptmann. The official name in Italian is Provincia autonoma di Bolzano — Alto Adige, South Tyrol as an administrative entity originated during the First World War. The Allies promised the area to Italy in the Treaty of London of 1915 as an incentive to enter the war on their side, with the rise of Fascism, the new regime made efforts to bring forward the Italianization of South Tyrol. The German language was banished from public service, German teaching was officially forbidden, the regime also favored immigration from other Italian regions. The subsequent alliance between Adolf Hitler and Benito Mussolini declared that South Tyrol would not follow the destiny of Austria, the region was de facto annexed to the German Reich until the end of the war. This status ended along with the Nazi regime, and Italian rule was restored in 1945, after the war the Allies decided that the province would remain a part of Italy, under the condition that the German-speaking population be granted a significant level of self-government. Italy and Austria negotiated an agreement in 1946, recognizing the rights of the German minority, alcide De Gasperi, Italys prime minister, a native of Trentino, wanted to extend the autonomy to his fellow citizens. This led to the creation of the region called Trentino-Alto Adige/Tiroler Etschland, German and Italian were both made official languages, and German-language education was permitted once more. Still Italians were the majority in the combined region, in a first phase, only public edifices and fascist monuments were targeted. The second phase was bloodier, costing 21 lives, the South Tyrolean question became an international issue. A fresh round of negotiations took place in 1961 but proved unsuccessful, the issue was resolved in 1971, when a new Austro-Italian treaty was signed and ratified
8.
Trentino
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Trentino, officially the Autonomous Province of Trento, is an autonomous province of Italy, in the countrys far north. Trentino is, along with South Tyrol, one of the two provinces making up the region of Trentino-Alto Adige/Südtirol, which is designated a region under the constitution. The province is divided into 178 comuni and its capital is the city of Trento. The province covers an area of more than 6,000 km2, Trentino is renowned for its mountains, such as the Dolomites, which are part of the Alps. The province is known as Trentino. The name derives from Trento, the city of the province. Originally, the term was used by the population only to refer to the city. In its wider sense, Trentino was first used around 1848 in an article by a member of the Frankfurt National Assembly, since the new 1972 autonomous status, the administrative name of the province is Autonomous Province of Trento. The history of Trentino begins in the mid-Stone Age, the valleys of what is now Trentino were already inhabited by man, the main settlements being in the valley of the Adige River, thanks to its milder climate. In the early Middle Ages, this area was included within the Kingdom of Italy, in 1027, the Bishopric of Trent was established as a State of the Holy Roman Empire by Emperor Conrad II. It was a territory, roughly corresponding to the present-day Trentino. The Council of Trent, held in three sessions from 1545 to 1563, with the first at Trento, was one of the important councils in the history of the Roman Catholic Church. It was an articulation of Roman Catholic doctrine in response to the Protestant Reformation, and specified doctrine on salvation, the sacraments, after the Napoleonic Wars of the early 19th century, the bishopric was secularized and absorbed into the Austrian County of Tyrol. It was governed by the House of Habsburg-Lorraine, the region was the location of heavy fighting during World War I, as it was directly on the front lines between Austria-Hungary and Italy. Trentino remained a part of Austria-Hungary until after the end of the war in 1919, since this treaty, Trentino enjoys considerable autonomy from the Italian central government in Rome. It has its own elected government and legislative assembly, in 1996, the Euroregion Tyrol-South Tyrol-Trentino was formed between the Austrian state of Tyrol and the Italian provinces of South Tyrol and Trentino. The boundaries of the association correspond to the old County of Tyrol, the aim is to promote regional peace, understanding and cooperation in many areas. The regions assemblies meet together as one on various occasions and have set up a liaison office to the European Union in Brussels
9.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
10.
Orogeny
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An Orogeny is an event that leads to a large structural deformation of the Earths lithosphere due to the interaction between tectonic plates. Orogens or orogenic belts develop when a plate is crumpled and is pushed upwards to form mountain ranges. Orogeny is the mechanism by which mountains are built on continents. The word orogeny comes from Ancient Greek, though it was used before him, the term was employed by the American geologist G. K. Gilbert in 1890 to describe the process of mountain building as distinguished from epeirogeny. Formation of an orogen is accomplished in part by the processes of subduction or convergence of two or more continents. Orogeny usually produces long arcuate structures, known as orogenic belts, generally, orogenic belts consist of long parallel strips of rock exhibiting similar characteristics along the length of the belt. Orogenic belts are associated with zones, which consume crust, produce volcanoes. Geologists attribute the arcuate structure to the rigidity of the descending plate and these island arcs may be added to a continent during an orogenic event. The processes of orogeny can take tens of millions of years, frequently, rock formations that undergo orogeny are severely deformed and undergo metamorphism. Orogenic processes may push deeply buried rocks to the surface, sea-bottom and near-shore material may cover some or all of the orogenic area. If the orogeny is due to two continents colliding, very high mountains can result, an orogenic event may be studied, as a tectonic structural event, as a geographical event, and as a chronological event. The foreland basin forms ahead of the orogen due mainly to loading and resulting flexure of the lithosphere by the mountain belt. The basin migrates with the front and early deposited foreland basin sediments become progressively involved in folding and thrusting. Sediments deposited in the basin are mainly derived from the erosion of the actively uplifting rocks of the mountain range. The fill of many such shows an change in time from deepwater marine through shallow water to continental sediments. Although orogeny involves plate tectonics, the tectonic forces result in a variety of associated phenomena, including magmatism, metamorphism, crustal melting, what exactly happens in a specific orogen depends upon the strength and rheology of the continental lithosphere, and how these properties change during orogenesis. In addition to orogeny, the orogen is subject to other processes, for example, the Caledonian Orogeny refers to the Silurian and Devonian events that resulted from the collision of Laurentia with Eastern Avalonia and other former fragments of Gondwana. The Caledonian Orogen resulted from events and various others that are part of its peculiar orogenic cycle
11.
Geologic time scale
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The table of geologic time spans, presented here, agrees with the nomenclature, dates and standard color codes set forth by the International Commission on Stratigraphy. Evidence from radiometric dating indicates that Earth is about 4.54 billion years old, the geology or deep time of Earth’s past has been organized into various units according to events which took place in each period. Older time spans, which predate the reliable record, are defined by their absolute age. Some other planets and moons within the Solar System have sufficiently rigid structures to have preserved records of their own histories, for example, Venus, Mars, dominantly fluid planets, such as the gas giants, do not preserve their history in a comparable manner. Apart from the Late Heavy Bombardment, events on other planets probably had little influence on the Earth. Construction of a scale that links the planets is, therefore, of only limited relevance to the Earths time scale. The existence, timing, and terrestrial effects of the Late Heavy Bombardment is still debated, the largest defined unit of time is the supereon, composed of eons. Eons are divided into eras, which are in turn divided into periods, epochs, the terms eonothem, erathem, system, series, and stage are used to refer to the layers of rock that correspond to these periods of geologic time in Earths history. Geologists qualify these units as early, mid, and late when referring to time, and lower, middle, for example, the lower Jurassic Series in chronostratigraphy corresponds to the early Jurassic Epoch in geochronology. The adjectives are capitalized when the subdivision is formally recognized, and lower case when not, thus early Miocene but Early Jurassic. Geologic units from the time but different parts of the world often look different and contain different fossils. For example, in North America the Lower Cambrian is called the Waucoban series that is subdivided into zones based on succession of trilobites. In East Asia and Siberia, the unit is split into Alexian, Atdabanian. A key aspect of the work of the International Commission on Stratigraphy is to reconcile this conflicting terminology, the term Anthropocene is used informally by popular culture and a growing number of scientists to describe the current epoch in which we are living. The term was coined by Paul Crutzen and Eugene Stoermer in 2000 to describe the current time, others say that humans have not even started to leave their biggest impact on Earth, and therefore the Anthropocene hasnt even started yet. Whatever the case, the ICS has not officially approved the term, leonardo da Vinci concurred with Aristotles interpretation that fossils represented the remains of ancient life. The 11th-century Persian geologist Avicenna and the 13th-century Dominican bishop Albertus Magnus extended Aristotles explanation into a theory of a petrifying fluid. Avicenna also first proposed one of the principles underlying geologic time scales, the Chinese naturalist Shen Kuo also recognized the concept of deep time
12.
Triassic
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The Triassic is a geologic period and system which spans 50.9 million years from the end of the Permian Period 252.17 million years ago, to the beginning of the Jurassic Period 201.3 Mya. The Triassic is the first period of the Mesozoic Era, both the start and end of the period are marked by major extinction events. Therapsids and archosaurs were the terrestrial vertebrates during this time. A specialized subgroup of archosaurs, called dinosaurs, first appeared in the Late Triassic, the vast supercontinent of Pangaea existed until the mid-Triassic, after which it began to gradually rift into two separate landmasses, Laurasia to the north and Gondwana to the south. The global climate during the Triassic was mostly hot and dry, however, the climate shifted and became more humid as Pangaea began to drift apart. The end of the period was marked by yet another mass extinction, the Triassic-Jurassic extinction event. The Triassic is usually separated into Early, Middle, and Late Triassic Epochs, from the east, along the equator, the Tethys sea penetrated Pangaea, causing the Paleo-Tethys Ocean to be closed. Later in the mid-Triassic a similar sea penetrated along the equator from the west, the remaining shores were surrounded by the world-ocean known as Panthalassa. All the deep-ocean sediments laid down during the Triassic have disappeared through subduction of oceanic plates, thus, the supercontinent Pangaea was rifting during the Triassic—especially late in that period—but had not yet separated. In North America, for example, marine deposits are limited to a few exposures in the west, thus Triassic stratigraphy is mostly based on organisms that lived in lagoons and hypersaline environments, such as Estheria crustaceans. At the beginning of the Mesozoic Era, Africa was joined with Earths other continents in Pangaea, Africa shared the supercontinents relatively uniform fauna which was dominated by theropods, prosauropods and primitive ornithischians by the close of the Triassic period. Late Triassic fossils are found throughout Africa, but are common in the south than north. The time boundary separating the Permian and Triassic marks the advent of an event with global impact. At Paleorrota geopark, located in Rio Grande do Sul, Brazil, in these formations, one of the earliest dinosaurs, Staurikosaurus, as well as the mammal ancestors Brasilitherium and Brasilodon have been discovered. The Triassic continental interior climate was hot and dry, so that typical deposits are red bed sandstones and evaporites. Pangaeas large size limited the effect of the global ocean, its continental climate was highly seasonal, with very hot summers. The strong contrast between the Pangea supercontinent and the global ocean triggered intense cross-equatorial monsoons, the best studied of such episodes of humid climate, and probably the most intense and widespread, was the Carnian Pluvial Event. On land, the vascular plants included the lycophytes, the dominant cycadophytes, ginkgophyta, ferns, horsetails
13.
Dolomite
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Dolomite is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally CaMg2. The term is used for a sedimentary carbonate rock composed mostly of the mineral dolomite. An alternative name used for the dolomitic rock type is dolostone. Most probably the mineral dolomite was first described by Carl Linnaeus in 1768, nicolas-Théodore de Saussure first named the mineral in March 1792. The mineral dolomite crystallizes in the trigonal-rhombohedral system and it forms white, tan, gray, or pink crystals. Dolomite is a carbonate, having an alternating structural arrangement of calcium and magnesium ions. It does not rapidly dissolve or effervesce in dilute hydrochloric acid as calcite does, solid solution exists between dolomite, the iron-dominant ankerite and the manganese-dominant kutnohorite. Small amounts of iron in the give the crystals a yellow to brown tint. Manganese substitutes in the structure also up to three percent MnO. A high manganese content gives the crystals a rosy pink color, lead, zinc, and cobalt also substitute in the structure for magnesium. The mineral dolomite is closely related to huntite Mg3Ca4, because dolomite can be dissolved by slightly acidic water, areas of dolomite are important as aquifers and contribute to karst terrain formation. Modern dolomite formation has been found to occur under conditions in supersaturated saline lagoons along the Rio de Janeiro coast of Brazil, namely, Lagoa Vermelha. It is often thought that dolomite will develop only with the help of sulfate-reducing bacteria, however, low-temperature dolomite may occur in natural environments rich in organic matter and microbial cell surfaces. This occurs as a result of magnesium complexation by carboxyl groups associated with organic matter, vast deposits of dolomite are present in the geological record, but the mineral is relatively rare in modern environments. Reproducible, inorganic low-temperature syntheses of dolomite and magnesite were published for the first time in 1999, the general principle governing the course of this irreversible geochemical reaction has been coined breaking Ostwalds step rule. There is some evidence for an occurrence of dolomite. One example is that of the formation of dolomite in the bladder of a Dalmatian dog. In 2015, it was discovered that the direct crystallization of dolomite can occur from solution at temperatures between 60 and 220 °C
14.
World Heritage Site
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A World Heritage Site is a landmark which has been officially recognized by the United Nations, specifically by the United Nations Educational, Scientific and Cultural Organization. Sites are selected on the basis of having cultural, historical, scientific or some form of significance. UNESCO regards these sites as being important to the interests of humanity. The programme catalogues, names, and conserves sites of outstanding cultural or natural importance to the common culture, under certain conditions, listed sites can obtain funds from the World Heritage Fund. The program was founded with the Convention Concerning the Protection of the Worlds Cultural and Natural Heritage, since then,192 state parties have ratified the convention, making it one of the most adhered to international instruments. As of July 2016,1052 sites are listed,814 cultural,203 natural, in 1959, the governments of Egypt and Sudan requested UNESCO to assist their countries to protect and rescue the endangered monuments and sites. In 1960, the Director-General of UNESCO launched an appeal to the Member States for an International Campaign to Save the Monuments of Nubia, the campaign, which ended in 1980, was considered a success. The project cost $80 million, about $40 million of which was collected from 50 countries, the projects success led to other safeguarding campaigns, saving Venice and its lagoon in Italy, the ruins of Mohenjo-daro in Pakistan, and the Borobodur Temple Compounds in Indonesia. UNESCO then initiated, with the International Council on Monuments and Sites, the United States initiated the idea of cultural conservation with nature conservation. The International Union for Conservation of Nature developed similar proposals in 1968, the Convention came into force on 17 December 1975. As of June 2016, it has been ratified by 192 states, including 188 UN member states plus the Cook Islands, the Holy See, Niue, a country must first list its significant cultural and natural sites, the result is called the Tentative List. A country may not nominate sites that have not been first included on the Tentative List, next, it can place sites selected from that list into a Nomination File. The Nomination File is evaluated by the International Council on Monuments and Sites and these bodies then make their recommendations to the World Heritage Committee. There are ten selection criteria – a site must meet at least one of them to be included on the list, up to 2004, there were six criteria for cultural heritage and four criteria for natural heritage. In 2005, this was modified so there is now only one set of ten criteria. Nominated sites must be of outstanding value and meet at least one of the ten criteria. Thus, the Geneva Convention treaty promulgates, Article 53, PROTECTION OF CULTURAL OBJECTS AND OF PLACES OF WORSHIP. There are 1,052 World Heritage Sites located in 165 States Party, of these,814 are cultural,203 are natural and 35 are mixed properties
15.
IUCN
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The International Union for Conservation of Nature is an international organization working in the field of nature conservation and sustainable use of natural resources. It is involved in gathering and analysis, research, field projects, advocacy, lobbying. IUCNs mission is to influence, encourage and assist societies throughout the world to conserve nature and to ensure that any use of resources is equitable. Over the past decades, IUCN has widened its focus beyond conservation ecology and now incorporates issues related to equality, poverty alleviation. Unlike other international NGOs, IUCN does not itself aim to mobilize the public in support of nature conservation and it tries to influence the actions of governments, business and other stakeholders by providing information and advice, and through lobbying and partnerships. The organization is best known to the public for compiling and publishing the IUCN Red List. IUCN has a membership of over 1200 governmental and non-governmental organizations, some 11,000 scientists and experts participate in the work of IUCN commissions on a voluntary basis. It employs approximately 1000 full-time staff in more than 60 countries and its headquarters are in Gland, Switzerland. IUCN has observer and consultative status at the United Nations, and plays a role in the implementation of several conventions on nature conservation. It was involved in establishing the World Wide Fund for Nature, in the past, IUCN has been criticized for placing the interests of nature over those of indigenous peoples. In recent years, its relations with the business sector have caused controversy. It was previously called the International Union for Protection of Nature, establishment In 1947, the Swiss League for the Protection of Nature organised an international conference on the protection of nature in Brunnen. It is considered to be the first government-organized non-governmental organization, the initiative to set up the new organisation came from UNESCO and especially from its first Director General, the British biologist Julian Huxley. At the time of its founding IUPN was the international organisation focusing on the entire spectrum of nature conservation Early years. Its secretariat was located in Brussels and its first work program focused on saving species and habitats, increasing and applying knowledge, advancing education, promoting international agreements and promoting conservation. Providing a solid base for conservation action was the heart of all activities. IUPN and UNESCO were closely associated and they jointly organized the 1949 Conference on Protection of Nature. In preparation for this conference a list of endangered species was drawn up for the first time
16.
National park
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A national park is a park in use for conservation purposes. Often it is a reserve of natural, semi-natural, or developed land that a sovereign state declares or owns, although individual nations designate their own national parks differently, there is a common idea, the conservation of wild nature for posterity and as a symbol of national pride. An international organization, the International Union for Conservation of Nature, although Yellowstone was not officially termed a national park in its establishing law, it was always termed such in practice and is widely held to be the first and oldest national park in the world. The first area to use national park in its legislation was the USs Mackinac Island. Australias Royal National Park, established in 1879, was the third official national park. In 1895 ownership of Mackinac Island was transferred to the State of Michigan as a state park, as a result, Australias Royal National Park is by some considerations the second oldest national park now in existence. The largest national park in the meeting the IUCN definition is the Northeast Greenland National Park. According to the IUCN,6,555 national parks worldwide met its criteria in 2006, IUCN is still discussing the parameters of defining a national park. National parks are almost always open to visitors, in 1971, these criteria were further expanded upon leading to more clear and defined benchmarks to evaluate a national park. In 1810, the English poet William Wordsworth described the Lake District as a sort of property, in which every man has a right and interest who has an eye to perceive. It was known as Hot Springs Reservation, but no authority was established. Federal control of the area was not clearly established until 1877, John Muir is today referred to as the Father of the National Parks due to his work in Yosemite. He published two articles in The Century Magazine, which formed the base for the subsequent legislation. President Abraham Lincoln signed an Act of Congress on July 1,1864, ceding the Yosemite Valley, according to this bill, private ownership of the land in this area was no longer possible. The state of California was designated to manage the park for use, resort. Leases were permitted for up to ten years and the proceeds were to be used for conservation, a public discussion followed this first legislation of its kind and there was a heated debate over whether the government had the right to create parks. The perceived mismanagement of Yosemite by the Californian state was the reason why Yellowstone at its establishment six years later was put under national control, in 1872, Yellowstone National Park was established as the United States first national park, being also the worlds first national park. In some European countries, however, national protection and nature reserves already existed, such as Drachenfels, Yellowstone was part of a federally governed territory
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Veneto
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Veneto or Venetia is one of the twenty regions of Italy. Its population is five million, ranking fifth in Italy. The regions capital and largest city is Venice, Veneto was part of the Roman Empire until the 5th century AD. Later, after a period, it was part of the Republic of Venice until 1797. Venice ruled for centuries one of the largest and richest maritime republics. The Statute of Veneto describes Venetians as a people, besides Italian, most inhabitants also speak Venetian. The region is home to a notable nationalist movement, the regions largest party is the Venetist/Padanist Liga Veneta, a founding member of Lega Nord. The current President of Veneto is Luca Zaia, elected in 2010 with 60. 2% of the vote and the support of Lega Nord, The People of Freedom, Veneto is the 8th largest region in Italy, with a total area of 18,398.9 km2. At its northernmost corner it borders also on Austria, the north-south extension of Veneto is 210 km from the Austrian border to the mouth of the River Po. By area, 29% of its surface is mountainous, the highest massif in the Dolomites is the Marmolada-massif at 3,342 m. Other dolomitic peaks are the Tre Cime di Lavaredo and the Pale di San Martino, the Venetian Prealps are not as high and range between 700 m and 2,200 m. Fossil deposits are abundant there. The plain itself is subdivided into the plain and the lower plain. The lower plain is both a mainstay of production and the most populated part of the region. Several rivers flow through the region, the Po, Adige, Brenta, Bacchiglione, Livenza, Piave, the eastern shore of the largest lake in Italy, Lake Garda, belongs to Veneto. The coastline covers approximately 200 km, of which 100 km are beaches, the coasts of the Adriatic Sea are characterised by the Venetian Lagoon, a flat terrain with ponds, marshes and islands. The Po Delta to the south features sandbars and dunes along the coastline, the inland portion contains cultivable land recently reclaimed by a system of canals and dykes. Fish ponds have been created there as well, the delta and the lagoon are a stopping-point for migratory birds
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Belluno
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Belluno listen, is a town and province in the Veneto region of northern Italy. Located about 100 kilometres north of Venice, Belluno is the capital of the province of Belluno, with its roughly 36,000 inhabitants, it is the largest populated area of Valbelluna. It is one of the 15 municipalities of the Dolomiti Bellunesi National Park, together with other Alpine towns, Belluno engages in the Alpine Town of the Year Association for the implementation of the Alpine Convention to achieve sustainable development in the Alpine Arc. Belluno was named Alpine Town of the Year in 1999, the ancient city of Belluno rises above a cliff spur near the confluence of the Torrente Ardo and the Piave River. To the north is the imposing Schiara range of the Dolomites, with the famous Gusela del Vescovà, to the south, the foothills of the Alps separate Belluno from the Venetian plain. Further to the south is the Nevegal, in the Castionese area, the average annual temperature in Belluno is 9 °C, and the average annual precipitation is 137 cm. The name of the city is derived from Celtic belo-dunum which means splendid hill, the name was inspired by the favorable position within the valley. It is conjectured that the population of the area that became Belluno was largely Venetic with a strong Celtic minority, however, as the Romans expanded northward into the Alps, the Celtic either emigrated or were absorbed. The people of the area swore friendship to Rome in the 225 BC conflict with the Gauls, founded perhaps around 220-200 BC the initial influence of Rome was military and commercial. Strategically located, the town protected cities to the south, Belluno also became a supplier of iron and copper. Already within the Roman sphere of influence, the town was juridically and polictically incorporated into the Roman Republic by the second century BC. Sometime between the death of Julius Caesar and the ascent of Augustus, Bellunum became a Roman municipium, the town was ruled by quattorviri juri dicendo, by quattorviri aedilicia potestate, and by a Council of Elders. Under Augustus, it part of Regio X Venetia et Histria. Among its citizens were Caius Flavius Hostilius and his wife Domitia, after the fall of the Western Roman Empire, it was ruled by the Lombards and the Carolingians, the famous Belluno Treasure in the British Museum dates from this period. From the late 9th century it was ruled by a count-bishop and it received a castle, later it was a possession of the Ghibelline family of the Ezzelino. After having longly contended the nearby territory with Treviso, in the end Belluno gave itself to the Republic of Venice, the city was thenceforth an important hub for the transport of lumber from the Cadore through the Piave river. After the fall of the Republic, Belluno was an Austrian possession, the cathedral was much damaged by the earthquake of 1873, which destroyed a considerable portion of the town, though the campanile stood firm. The Duomo, with the 18th-century bell tower designed by Filippo Juvarra and it includes five paintings by Andrea Schiavone, three by Sebastiano Ricci
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Ladin language
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Ladin is a Romance language consisting of a group of dialects mainly spoken in the Dolomite Mountains in Northern Italy in South Tyrol, the Trentino and the province of Belluno by the Ladin people. It exhibits similarities to Swiss Romansh and Friulian, the precise extension of the Ladin language area is the subject of scholarly debates. Ladin should not be confused with Ladino, which, although also Romance, is derived from Old Spanish, Ladin is recognized as a minority language in 54 Italian municipalities belonging to the provinces of South Tyrol, Trentino and Belluno. In the 2011 census,20,548 inhabitants of South Tyrol declared Ladin as their native language, Ladin is an officially recognised language, taught in schools and used in public offices. The following municipalities of South Tyrol have a majority of Ladin speakers and they are spoken in 38 municipalities, but have no official status. Their more precise classification is uncertain, both dialects show a strong resemblance to Trentinian dialect and Eastern Lombard, and scholars debate whether they are Ladin dialects or not. About 23% of the inhabitants from Val di Non and 1. 5% from Val di Sole declared Ladin as their language at the 2011 census. The number of Ladin speakers in those valleys amounts to 8,730, in order to stress the difference between the dialects in Non and Fassa valleys, it has been proposed to distinguish between ladins dolomitiches and ladins nonejes at the next census. As there is no census in the province of Belluno. The provincial administration of Belluno has enacted to identify Ladin as a minority language in additional municipalities, ladinity in the province of Belluno is more ethnic than linguistic. The varieties spoken by Ladin municipalities are Venetian alpine dialects, grammatically no different to those spoken in municipalities that did not declare themselves as Ladin and their language is called Ladino Bellunese. All Ladin dialects spoken in the province of Belluno, including those in the former Tyrolean territories, the name derives from Latin, because Ladin is originally a Vulgar Latin language left over from the Romanized Alps. Ladin is often attributed to be a relic of Vulgar Latin dialects associated with Rhaeto-Romance languages, whether a proto-Romance language ever existed is controversially discussed amongst linguists and historians, a debate known as Questione Ladina. Starting in the 6th century, the Bavarii started moving in from the north, while from the south Gallo-Italic languages started pushing in, only in the more remote mountain valleys did Ladin survive among the isolated populations. Starting in the very early Middle Ages, the area was ruled by the County of Tyrol or the Bishopric of Brixen. The area of Cadore was under the rule of the Republic of Venice, during the period of the Holy Roman Empire of the German Nation and, after 1804, the Austrian Empire, the Ladins underwent a process of Germanization. After the end of World War I in 1918, Italy annexed the part of Tyrol. The programme of Italianization, professed by fascists such as Ettore Tolomei and Benito Mussolini and this included changing Ladin place names into the Italian pronunciation according to Tolomeis Prontuario dei nomi locali dellAlto Adige
20.
Venetian language
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It is sometimes spoken and often well understood outside Veneto, in Trentino, Friuli, Venezia Giulia, Istria, and some towns of Dalmatia, Croatia, Slovenia, Montenegro, Brazil, Mexico, and Romania. Although referred to as an Italian dialect even by its speakers and its precise place within the Romance language family is controversial, see below. Like all Italian dialects in the Romance language family, Venetian is descended from Vulgar Latin, Venetian is attested as a written language in the 13th century. There are also influences and parallelisms with Greek and Albanian in words such as pirón, inpiràr, caréga, the language enjoyed substantial prestige in the days of the Venetian Republic, when it attained the status of a lingua franca in the Mediterranean. Notable Venetian-language authors include the playwrights Ruzante, Carlo Goldoni and Carlo Gozzi, following the old Italian theatre tradition, they used Venetian in their comedies as the speech of the common folk. They are ranked among the foremost Italian theatrical authors of all time, other notable works in Venetian are the translations of the Iliad by Casanova and Francesco Boaretti, and the poems of Biagio Marin. However, as a literary language Venetian was overshadowed by Dantes Tuscan dialect and languages of France like Occitan, virtually all modern Venetian speakers are diglossic with Italian. The present situation raises questions about the medium term survival. Despite recent steps to recognize it, Venetian remains far below the threshold of inter-generational transfer with younger generations preferring standard Italian in many situations, the dilemma is further complicated by the ongoing large-scale arrival of immigrants, who only speak or learn standard Italian. In the past, however, Venetian spread to other continents as a result of migration from the Veneto region between 1870 and 1905 and 1945 and 1960. Tens of thousands of peasants and craftsmen were thrown off their lands or out of their workshops, Venetian migrants created large Venetian-speaking communities in Argentina, Brazil, and Mexico, where the language is still spoken today. Internal migrations under the Fascist regime also sent many Venetian speakers to other regions of Italy, currently, some firms have chosen to use the Venetian language in advertising as a famous beer did some years ago. Venetian is spoken mainly in the Italian regions of Veneto and Friuli-Venezia Giulia, smaller communities are found in Lombardy, Trentino, Emilia-Romagna, Sardinia, Lazio, and formerly in Romania. It is also spoken in North and South America by the descendants of Italian immigrants, in Mexico, the Chipilo Venetian dialect is spoken in the state of Puebla and the town of Chipilo. The town was settled by immigrants from the Veneto region, people from Chipilo have gone on to make satellite colonies in Mexico, especially in the states of Guanajuato, Querétaro, and State of Mexico. Venetian has also survived in the state of Veracruz, where other Italian migrants have settled from the late 1800s, the people of Chipilo preserve their dialect and call it chipileño and it has been preserved as a variant since the 19th century. The variant of the Venetan language spoken by the Cipiłàn is northern Trevisàn-Feltrìn-Belumàt, in 2009, the Brazilian city of Serafina Corrêa, in the state of Rio Grande do Sul, gave Talian a joint official status alongside Portuguese. Until the middle of the 20th century, Venetian was also spoken on the Greek Island of Corfu, which had long been under the rule of the Republic of Venice
21.
Friulian language
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Friulian or Friulan is a Romance language belonging to the Rhaeto-Romance family, spoken in the Friuli region of northeastern Italy. Friulian has around 600,000 speakers, the vast majority of whom also speak Italian, documents in Friulian are attested from the 11th century and poetry and literature date as far back as 1300. By the 20th century, there was a revival of interest in the language that has continued to this day, in North America the more common English form is Friulan for both the language and the ethnic identity of the people living in Friuli and abroad. Friulan follows the example of Friulano in Italian, see the reference, Friulan Dictionary, English-Friulan / Friulan-English. A question which causes many debates is the influence of the Latin spoken in Aquileia, some claim that it had peculiar features that later passed into Friulian. 357, wrote a commentary to the Gospel in sermo rusticus, in the language spoken by the people, the language spoken before the arrival of the Romans in 181 BC was of Celtic origin since the inhabitants belonged to the Carni, a Celtic population. In modern Friulian, the words of Celtic origins are many, even influences from the Lombard language - Friuli was one of their strongholds - are very frequent. In Friulian there are also a lot of German, Slovenian and Venetian words, from that evidence, scholars today agree that the formation of Friulian dates back to around 1000, at the same time as other dialects derived from Latin. The first written records of Friulian have been found in administrative acts of the 13th century, but the documents became more frequent in the following century, the main centre at that time was Cividale. The Friulian language has never acquired official status, legal statutes were first written in Latin, then in Venetian, the idea of unity among Ladin, Romansh and Friulian comes from the Italian historical linguist Graziadio Isaia Ascoli, who was born in Gorizia. In 1871, he presented his theory that three languages are part of one family, which in the past stretched from Switzerland to Muggia. The three languages are the survivors of this family and all developed differently. Friulian was much influenced by German. Many features that Ascoli thought were peculiar to the Rhaeto-Romance languages can, in fact, in the past, the language borders were wider since in Trieste and Muggia, local variants of Friulian were spoken. The main document about the dialect of Trieste, or tergestino, is Dialoghi piacevoli in dialetto vernacolo triestino, Friuli was, until the 1960s, an area of deep poverty, causing a large number of Friulian speakers to emigrate. Most went to France, Belgium, and Switzerland or outside Europe, to Canada, Mexico, Australia, Argentina, Brazil, Venezuela, the United States, in those countries, there are associations of Friulian immigrants that try to protect their traditions and language. The first texts in Friulian date back to the 13th century and are commercial or juridical acts. The examples show that Friulian was used together with Latin, which was still the administrative language, the most notable work is Piruç myò doç inculurit, it was composed by an anonymous author from Cividale del Friuli, probably in 1380
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Adige
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The river sources near the Reschen Pass close to the borders with Austria and Switzerland above the Inn valley. It flows through the artificial alpine Lake Reschen, the lake is known for the church tower that marks the site of the former village of Alt Graun, it was evacuated and flooded in 1953 after the dam was finished. Near Glurns, the Rom river joins from the Swiss Val Müstair, the Adige runs eastbound through the Vinschgau to Merano, where it is met by the Passer river from the north. The section between Merano and Bolzano, is called Etschtal, meaning Adige Valley, the Chiusa di Salorno narrows at Salorno mark the southernmost part of the predominantly German-speaking province of South Tyrol. The Adige was mentioned in the Lied der Deutschen of 1841 as the border of the German language area. In 1922 Germany adopted the song as its anthem, although by that time Italy had taken control of all of the Adige. Near Trento, the Avisio, Noce, and Fersina rivers join, the Adige crosses Trentino and later Veneto, flowing past the town of Rovereto, the Lagarina Valley, the cities of Verona and Adria and the north-eastern part of the Po Plain into the Adriatic Sea. The Adige and the Po run parallel in the river delta without properly joining, the Adige is connected to Lake Garda by the Mori-Torbole tunnel, an artificial underground canal built for flood prevention. The Adige is a home to the Marble trout, but at far lower populations than in the past, fish stocking is one of the most significant causes of the sharp reduction in the original fish population of this subspecies. It will spawn with and interbreed with brown trout, which are stocked in the river
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Piave River
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The Piave is a river in northern Italy. It begins in the Alps and flows southeast for 220 kilometres into the Adriatic Sea near the city of Venice, one of its tributaries is the Boite. In 1809 it was the scene of a battle during the Napoleonic Wars, in 1918, during World War I, it was the scene of Battle of the Piave River, the last major Austro-Hungarian attack on the Italian Front, which failed. The Battle of the Piave was the battle of World War I on the Italian Front. The river is called in Italy Fiume Sacro alla Patria and is mentioned in the patriotic song La leggenda del Piave. North of the city of Venice along the Piave river valley is the Denominazione di origine controllata zone that makes up the Veneto wine region known as the Piave DOC. Here both red and white wine is produced, mostly as varietal wines, with Merlot being the dominant grape of the region. Among the other grapes grown in the region are Cabernet Sauvignon, Cabernet franc, Pinot blanc, Pinot grigio, Pinot nero, Raboso, Friulano, Verduzzo Trevigiano and Verduzzo Friulano. The finished wines also must meet a minimum alcohol level—11. 5% for all varieties except Merlot and Friulano which only need to reach 11% alcohol by volume. A separate riserva bottling for the red varieties are permitted provided the wine is aged at least two years prior to release and attain a minimum alcohol level of at least 12. 5%. Site of italian newspaper Il Piave Official website of Consorzio Tutela Vini del Piave DOC - Consorzio Vini Venezia
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Pieve di Cadore
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Pieve di Cadore is a comune in the province of Belluno in the Italian region of Veneto, about 110 kilometres north of Venice and about 35 km northeast of Belluno. It is the birthplace of the Italian painter Titian, with its strategic location, the town was a medieval stronghold with fortifications, called the walled city of the Veneto. The main sight is the Palazzo della Magnifica Comunità, built in 1447 by the council which then ruled the city. It has a tower which was completed in 1491. A highway, SS51, connects the town with other communities in the Cadore Dolomite region, the town has a swimming pool, tennis club, ice hockey arena, a bocce stadium, soccer fields and a biking trail called Ciclabile delle Dolomiti with amazing views. The route of the 2013 Giro dItalia passed through Calalzo di Cadore during Stage 11, Titian - Italian Renaissance painter, born in Pieve di Cadore Official website Old postcards from Tai di Cadore
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Puster Valley
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The Puster Valley is a valley in the Alps that runs in an east-west direction between Lienz in East Tyrol, Austria and Mühlbach near Brixen in South Tyrol, Italy. The municipalities of the Puster Valley constitute the Puster Valley district, East of Sillian, the Puster Valley leaves the Peradriatic Line and turns to the northeast towards Lienz. Half of the valley drains to the west to the Adriatic via the Adige river, the watershed lies in the shallow valley floor called Toblacher Feld. The Rienz river flows westwards through the Puster Valley and the Drau river flows eastwards into East Tyrol, the eastern part of the valley on the upper Drava is called Upper Puster Valley. The towns in the Puster Valley are located between 750 and 1,180 meters above sea level. The most important of these towns in the valley are Toblach, Welsberg-Taisten, Olang, and Bruneck, the most important in the eastern valley are Innichen, Sexten. The largest tributaries of the Rienz river form the Antholzer Bach, the Ahr, the Pragser Bach, the Gsieser Bach, the Gran Ega, the Pfunderer Bach, the Puster Valleys largest side valley is the Tauferer Ahrntal. The Draus largest eastern tributaries are the Sextner Bach and the Villgraten-Bach, the Puster Valley District was founded in 1969 with the merger of 26 municipalities. Its combined area is 2,071 km² and its population is over 73,000, according to the 2001 census,80. 96% of the population of the valley speak German,13. 40% Ladin, and 5. 64% Italian as their native language. The following municipalities are part of the Puster Valley District, Media related to Puster Valley at Wikimedia Commons Puster Valley District
26.
Brenta Group
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The Brenta Group or Brenta Dolomites is a mountain range, and a subrange of the Rhaetian Alps in the Southern Limestone Alps mountain group. They are located in the Province of Trentino, in northeastern Italy and it is the only dolomitic group west of river Adige. Therefore, geographically, they have not always considered a part of the Dolomites mountain ranges. Geologically, however, they definitely are - and therefore called the Western Dolomites. As part of the Dolomites, the Brenta Group has been recognized as UNESCO World Heritage Site under the World Heritage Convention. Geologically, the Brenta Group is very different from the neighboring mountain groups like Ortles. The main peaks are formed of hard compact dolomite, while the peripheral subgroups often are made up of more calcareous dolomite or limestone, the hard dolomite was originally formed during the Mesozoic era, under the surface of the shallow Tethys Ocean, some 200 million years ago. The hard compact dolomite with a high magnesium content was formed during the Upper Triassic period, the softer, more calcareous material was deposited later, in the late Triassic and early Jurassic period. The difference is noticeable for the climber who gets a much more compact. Subsequent erosion carved out the landscape with its steep vertical pinnacles. Traditionally, the Brenta glaciers were relatively small and called vedrette, over the last hundred years their size has been reduced to often smaller than half of their original size around 1900. Climate change appears to be the main reason, the Brenta Group covers a relatively large area. Northern Sector comprising the Northern chain and the subgroup of La Campa, the Brenta Group counts a number of lakes of which the Molveno Lake and the Tovèl Lake are the most significant. Notable peaks of the Brenta Group are, Recent research has suggested that Cima Tosa is not as high as 3173 metres and is lower than Cima Brenta. A year later he reached the summit of the Cima Tosa, only to find out that a few days earlier, on July 20,1865, ball wrote about his endeavors in the Alpine Journal and attracted other British explorers to the Brenta Group. Douglas Freshfield, a chairman of the prestigious Alpine Club arrived in 1871. He and his companions Francis Fox Tuckett and the French guide François Devouassoud from Chamonix and these men, who all would become main figures of the Golden Age of Alpinism were active in the Brenta Group and Presanella in 1871 and 1872. In 1871 they reached the summit of the Cima Brenta, other British mountaineers of that era that would add to the exploration of the Brenta Group were Arthur John Butler, Albert de Falkner and Edward Theodore Compton
27.
Province of Verona
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The Province of Verona is a province in the Veneto region of Italy. The eastern bank of Lake Garda is near the province and its capital is the city of Verona. The city is a UNESCO World Heritage Site, the province is cosmopolitan in nature. It is bordered by Italian Tyrol in the north, Province of Vicenza, Province of Rovigo and Province of Mantua in south and Lake Garda in the west. From north to south the maximum extent of the province is 50 miles while it is 25 miles from east to west, the province has an area of 3,109 square kilometres and a total population of about 0.9 million. There are 98 comuni in the province, william Shakespeares play Romeo and Juliet takes place in Verona, as do some scenes in his play The Two Gentlemen of Verona. The Casa di Giulietta is an important local visitor attraction, Verona attracts a large number of tourists every year. Due to its important role in history the province boasts of a number of castles, towers, hermitages, monasteries, sanctuaries. A regional park is located in Lessinia, valpolicella is popular for its wines which are made from indigenous techniques. Europes biggest natural bridge-Ponte di Veja is located in the province, the northern part of the province is mostly hilly. Several rivers pass through the rivers, a few of them are Tartaro, Caslagnaro and Adige. Media related to Province of Verona at Wikimedia Commons Tourist information
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Province of Vicenza
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The Province of Vicenza is a province in the Veneto region of northern Italy. The province has an area of 2,723 km², there are 121 comuni in the province. Important towns in the province include Bassano del Grappa, Montecchio Maggiore, Torri di Quartesolo, Schio, Noventa Vicentina, Thiene, Marostica, Lonigo, Arzignano, the provinces president, since 2014, is Achille Variati of the Democratic Party. The provinces president, from 2007 to 2014, was Attilio Schneck of the Liga Veneta party, Liga Veneta is a member of the Lega Nord. group of political parties that, in turn, is part of the center-right coalition. Before him, the president was Manuela Dal Lago, also a member of the Liga Veneta, population is unevenly spread throughout the province. More than 60% of the populace resides in densely industrialised areas in the eastern, western, the remaining 40% reside in predominantly rural ares in the southern part of the province or the Asiago plateau. Economic development in areas is hindered by industrial and agricultural depression. The heavily industrial Alto Vicentino area alone accounts for half of the provinces GDP, indias most influential woman, Sonia Gandhi, the widow of former prime minister Rajiv Gandhi, was born in the province of Vicenza. She currently resides in New Delhi and she was named the third-most powerful woman in the world by Forbes magazine in the year 2004 and currently ranks sixth. She was also named among Time magazines 100 Most Influential People in the World for the years 2007 and 2008, the famous inventor Federico Faggin, an Italian physicist/electrical engineer principally responsible for the design of the first microprocessor, was born in Vicenza. Calà del Sasso Strada delle 52 Gallerie Provincia di Vicenza homepage Guide to Outdoor Activities in the Vicenza Province
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UNESCO World Heritage Site
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A World Heritage Site is a landmark which has been officially recognized by the United Nations, specifically by the United Nations Educational, Scientific and Cultural Organization. Sites are selected on the basis of having cultural, historical, scientific or some form of significance. UNESCO regards these sites as being important to the interests of humanity. The programme catalogues, names, and conserves sites of outstanding cultural or natural importance to the common culture, under certain conditions, listed sites can obtain funds from the World Heritage Fund. The program was founded with the Convention Concerning the Protection of the Worlds Cultural and Natural Heritage, since then,192 state parties have ratified the convention, making it one of the most adhered to international instruments. As of July 2016,1052 sites are listed,814 cultural,203 natural, in 1959, the governments of Egypt and Sudan requested UNESCO to assist their countries to protect and rescue the endangered monuments and sites. In 1960, the Director-General of UNESCO launched an appeal to the Member States for an International Campaign to Save the Monuments of Nubia, the campaign, which ended in 1980, was considered a success. The project cost $80 million, about $40 million of which was collected from 50 countries, the projects success led to other safeguarding campaigns, saving Venice and its lagoon in Italy, the ruins of Mohenjo-daro in Pakistan, and the Borobodur Temple Compounds in Indonesia. UNESCO then initiated, with the International Council on Monuments and Sites, the United States initiated the idea of cultural conservation with nature conservation. The International Union for Conservation of Nature developed similar proposals in 1968, the Convention came into force on 17 December 1975. As of June 2016, it has been ratified by 192 states, including 188 UN member states plus the Cook Islands, the Holy See, Niue, a country must first list its significant cultural and natural sites, the result is called the Tentative List. A country may not nominate sites that have not been first included on the Tentative List, next, it can place sites selected from that list into a Nomination File. The Nomination File is evaluated by the International Council on Monuments and Sites and these bodies then make their recommendations to the World Heritage Committee. There are ten selection criteria – a site must meet at least one of them to be included on the list, up to 2004, there were six criteria for cultural heritage and four criteria for natural heritage. In 2005, this was modified so there is now only one set of ten criteria. Nominated sites must be of outstanding value and meet at least one of the ten criteria. Thus, the Geneva Convention treaty promulgates, Article 53, PROTECTION OF CULTURAL OBJECTS AND OF PLACES OF WORSHIP. There are 1,052 World Heritage Sites located in 165 States Party, of these,814 are cultural,203 are natural and 35 are mixed properties
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Carbonate rock
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Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone, which is composed of calcite or aragonite and dolostone, which is composed of the mineral dolomite. Calcite can be dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH. Calcite exhibits a characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases. When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures, karst topography and caves develop in carbonate rocks because of their solubility in dilute acidic groundwater. Cooling groundwater or mixing of different groundwaters will also create conditions suitable for cave formation, marble is the metamorphic carbonate rock. Rare igneous carbonate rocks exist as intrusive carbonatites and even rarer volcanic carbonate lava
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Dolostone
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Dolostone or dolomite rock is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg2. In old USGS publications it was referred to as magnesian limestone, technically, dolostone has a stoichiometric ratio of nearly equal amounts of magnesium and calcium. Most dolostones formed as a replacement of limestone or lime mud prior to lithification. It is resistant to erosion and can either contain bedded layers or be unbedded and it is less soluble than limestone in weakly acidic groundwater, but it can still develop solution features over time. Dolostone can act as an oil and natural gas reservoir, the term dolostone was introduced to avoid confusion with the mineral dolomite. The usage of the term dolostone is controversial because the name dolomite was first applied to the rock during the late 18th century, the use of the term dolostone is not recommended by the Glossary of Geology published by the American Geological Institute. It is, however, used in some geological publications, the geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The dolomite problem refers to the vast worldwide depositions of dolostone in past geologic record eluding a unified explanation for their formation, as with limestone caves, natural caves and solution tubes can form in dolomite rock as a result of dissolution by weak carbonic acid. Calcium carbonate speleothems in the forms of stalactites, stalagmites, flowstone etc, “Dolomite is a common rock type, but a relatively uncommon mineral in speleothems”. Both calcium and magnesium go into solution when dolomite rock is dissolved, the speleothem precipitation sequence is, calcite, Mg-calcite, aragonite, huntite and hydromagnesite. Hence, the most common speleothem in caves within dolomite rock karst, is calcium carbonate in the most stable form of calcite. Speleothem types known to have a dolomite constituent include, coatings, crusts, moonmilk, flowstone, coralloids, powder, spar and rafts. Although there are reports of dolomite speleothems known to exist in a number of cave around the world, they are usually in small quantities. Blatt, Harvey, Tracy, Robert J. Petrology, Igneous, Sedimentary, tucker, M. E. V. P. Wright. Zenger, D. H. Mazzullo, S. J. Dolomitization
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Mineralogy
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Mineralogy is a subject of geology specializing in the scientific study of chemistry, crystal structure, and physical properties of minerals and mineralized artifacts. Specific studies within mineralogy include the processes of mineral origin and formation, classification of minerals, their geographical distribution, the German Renaissance specialist Georgius Agricola wrote works such as De re metallica and De Natura Fossilium which began the scientific approach to the subject. Systematic scientific studies of minerals and rocks developed in post-Renaissance Europe, the modern study of mineralogy was founded on the principles of crystallography and to the microscopic study of rock sections with the invention of the microscope in the 17th century. Nicholas Steno first observed the law of constancy of interfacial angles in quartz crystals in 1669 and this was later generalized and established experimentally by Jean-Baptiste L. Romé de lIslee in 1783. In 1814, Jöns Jacob Berzelius introduced a classification of minerals based on their chemistry rather than their crystal structure, james D. Dana published his first edition of A System of Mineralogy in 1837, and in a later edition introduced a chemical classification that is still the standard. It, however, retains a focus on the structures commonly encountered in rock-forming minerals. An initial step in identifying a mineral is to examine its physical properties and these can be classified into density, measures of mechanical cohesion, macroscopic visual properties, magnetic and electric properties, radioactivity and solubility in hydrogen chloride. If the mineral is crystallized, it will also have a distinctive crystal habit that reflects the crystal structure or internal arrangement of atoms. It is also affected by crystal defects and twinning. Many crystals are polymorphic, having more than one crystal structure depending on factors such as pressure and temperature. ”Examples of polymorphs are calcite and aragonite - two minerals with identical chemical composition, distinguished by their crystallography, calcite is rhombohedral and aragonite is orthorhombic. The crystal structure is the arrangement of atoms in a crystal and it is represented by a lattice of points which repeats a basic pattern, called a unit cell, in three dimensions. The lattice can be characterized by its symmetries and by the dimensions of the unit cell and these dimensions are represented by three Miller indices. The lattice remains unchanged by certain symmetry operations about any point in the lattice, reflection, rotation, inversion, and rotary inversion. Together, they make up an object called a crystallographic point group or crystal class. There are 32 possible crystal classes, in addition, there are operations that displace all the points, translation, screw axis, and glide plane. In combination with the point symmetries, they form 230 possible space groups, most geology departments have X-ray powder diffraction equipment to analyze the crystal structures of minerals. X-rays have wavelengths that are the order of magnitude as the distances between atoms. In a sample that is ground to a powder, the X-rays sample a random distribution of all crystal orientations, powder diffraction can distinguish between minerals that may appear the same in a hand sample, for example quartz and its polymorphs tridymite and cristobalite
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World War I
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World War I, also known as the First World War, the Great War, or the War to End All Wars, was a global war originating in Europe that lasted from 28 July 1914 to 11 November 1918. More than 70 million military personnel, including 60 million Europeans, were mobilised in one of the largest wars in history and it was one of the deadliest conflicts in history, and paved the way for major political changes, including revolutions in many of the nations involved. The war drew in all the worlds great powers, assembled in two opposing alliances, the Allies versus the Central Powers of Germany and Austria-Hungary. These alliances were reorganised and expanded as more nations entered the war, Italy, Japan, the trigger for the war was the assassination of Archduke Franz Ferdinand of Austria, heir to the throne of Austria-Hungary, by Yugoslav nationalist Gavrilo Princip in Sarajevo on 28 June 1914. This set off a crisis when Austria-Hungary delivered an ultimatum to the Kingdom of Serbia. Within weeks, the powers were at war and the conflict soon spread around the world. On 25 July Russia began mobilisation and on 28 July, the Austro-Hungarians declared war on Serbia, Germany presented an ultimatum to Russia to demobilise, and when this was refused, declared war on Russia on 1 August. Germany then invaded neutral Belgium and Luxembourg before moving towards France, after the German march on Paris was halted, what became known as the Western Front settled into a battle of attrition, with a trench line that changed little until 1917. On the Eastern Front, the Russian army was successful against the Austro-Hungarians, in November 1914, the Ottoman Empire joined the Central Powers, opening fronts in the Caucasus, Mesopotamia and the Sinai. In 1915, Italy joined the Allies and Bulgaria joined the Central Powers, Romania joined the Allies in 1916, after a stunning German offensive along the Western Front in the spring of 1918, the Allies rallied and drove back the Germans in a series of successful offensives. By the end of the war or soon after, the German Empire, Russian Empire, Austro-Hungarian Empire, national borders were redrawn, with several independent nations restored or created, and Germanys colonies were parceled out among the victors. During the Paris Peace Conference of 1919, the Big Four imposed their terms in a series of treaties, the League of Nations was formed with the aim of preventing any repetition of such a conflict. This effort failed, and economic depression, renewed nationalism, weakened successor states, and feelings of humiliation eventually contributed to World War II. From the time of its start until the approach of World War II, at the time, it was also sometimes called the war to end war or the war to end all wars due to its then-unparalleled scale and devastation. In Canada, Macleans magazine in October 1914 wrote, Some wars name themselves, during the interwar period, the war was most often called the World War and the Great War in English-speaking countries. Will become the first world war in the sense of the word. These began in 1815, with the Holy Alliance between Prussia, Russia, and Austria, when Germany was united in 1871, Prussia became part of the new German nation. Soon after, in October 1873, German Chancellor Otto von Bismarck negotiated the League of the Three Emperors between the monarchs of Austria-Hungary, Russia and Germany
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Austro-Hungary
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The union was a result of the Austro-Hungarian Compromise of 1867 and came into existence on 30 March 1867. Austria-Hungary consisted of two monarchies, and one region, the Kingdom of Croatia-Slavonia under the Hungarian crown. It was ruled by the House of Habsburg, and constituted the last phase in the evolution of the Habsburg Monarchy. Following the 1867 reforms, the Austrian and the Hungarian states were co-equal, Foreign affairs and the military came under joint oversight, but all other governmental faculties were divided between respective states. Austria-Hungary was a state and one of the worlds great powers at the time. Austria-Hungary was geographically the second-largest country in Europe after the Russian Empire, at 621,538 km2, the Empire built up the fourth-largest machine building industry of the world, after the United States, Germany, and the United Kingdom. After 1878, Bosnia and Herzegovina was under Austro-Hungarian military and civilian rule until it was annexed in 1908. The annexation of Bosnia also led to Islam being recognized as a state religion due to Bosnias Muslim population. Austria-Hungary was one of the Central Powers in World War I and it was already effectively dissolved by the time the military authorities signed the armistice of Villa Giusti on 3 November 1918. The realms full, official name was The Kingdoms and Lands Represented in the Imperial Council, each enjoyed considerable sovereignty with only a few joint affairs. Certain regions, such as Polish Galicia within Cisleithania and Croatia within Transleithania, enjoyed autonomous status, the division between Austria and Hungary was so marked that there was no common citizenship, one was either an Austrian citizen or a Hungarian citizen, never both. This also meant that there were always separate Austrian and Hungarian passports, however, neither Austrian nor Hungarian passports were used in the Kingdom of Croatia-Slavonia-Dalmatia. Instead, the Kingdom issued its own passports which were written in Croatian and French and it is not known what kind of passports were used in Bosnia-Herzegovina, which was under the control of both Austria and Hungary. The Kingdom of Hungary had always maintained a separate parliament, the Diet of Hungary, the administration and government of the Kingdom of Hungary remained largely untouched by the government structure of the overarching Austrian Empire. Hungarys central government structures remained well separated from the Austrian imperial government, the country was governed by the Council of Lieutenancy of Hungary – located in Pressburg and later in Pest – and by the Hungarian Royal Court Chancellery in Vienna. The Hungarian government and Hungarian parliament were suspended after the Hungarian revolution of 1848, despite Austria and Hungary sharing a common currency, they were fiscally sovereign and independent entities. Since the beginnings of the union, the government of the Kingdom of Hungary could preserve its separated. After the revolution of 1848–1849, the Hungarian budget was amalgamated with the Austrian, from 1527 to 1851, the Kingdom of Hungary maintained its own customs controls, which separated her from the other parts of the Habsburg-ruled territories
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Via ferrata
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A via ferrata is a protected climbing route found in the Alps and certain other locations. The essence of a modern via ferrata is a cable which runs along the route and is periodically fixed to the rock. Using a via ferrata kit, climbers can secure themselves to the cable, the cable can also be used as aid to climbing, and additional climbing aids, such as iron rungs, pegs, carved steps and even ladders and bridges are often provided. Thus via ferratas allow otherwise dangerous routes to be undertaken without the associated with unprotected scrambling and climbing or the need for climbing equipment such as ropes. Conversely, the modest equipment requirements, ability to do them solo, via ferratas can vary in length from short routes taking less than an hour, to long, demanding alpine routes covering significant distance and altitude, and taking eight or more hours to complete. Generally, via ferratas are done in ascent, although it is possible to descend them, many more have been developed in recent years, as their popularity has grown and the tourism benefits have been recognised. Over 1000 via ferratas now exist, the majority are found in the Alps, most notably in Italy and Austria. Others are found in a number of European countries, and a few places elsewhere, however, they are now found in a range of different terrains. The term via ferrata is used in most countries and languages, except notably in German-speaking countries which use Klettersteig, simple protected paths, with ladders and basic protection aids, have probably existed in the Alps for centuries, helping to connect villages to their high pastures. Construction of what could be seen as the precursors of modern via ferratas dates back to the growth of Alpine exploration and tourism in the nineteenth century. In 1843, a route on the Dachstein was constructed under the direction of Friedrich Simony, it included a range of climbing aids with iron pins, hand hooks, carved footholds and ropes. In 1869 a rope was fixed between the summits of Grossglockner, and in 1873 fixed protection was installed on the Zugspitze, in the Pyrenees, iron climbing aids were installed on the Pic du Midi dOssau in 1880, and in the Ordesa in 1881. In the Dolomites, the path up the West ridge of the Marmolada was installed in 1903. In 1914 the Dolomites were part of the Austro-Hungarian Empire, which was part of the Central Powers during the First World War, in 1915, Italy joined the alliance of Britain, France, and Russia and declared war on the Central Powers. Austria’s troops were committed in Russia and it immediately withdrew to a defensive line which ran through the Dolomites. Until the end of 1917 the Austrians and the Italians fought a war in the mountains of the Dolomites, not only against each other. Both sides tried to control of the peaks to site observation posts. To help troops move about at high altitude in very difficult conditions, permanent lines were fixed to rock faces and they also tried to create and control tunnels below the peaks to attack from there
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Alta Via 1
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Alta Via 1 is a 150-kilometre-long high-level public footpath which runs through the eastern Dolomites in Italy. It is also known as the Dolomite High Route 1 and it passes through some of the finest scenery in the Dolomites. The path runs south from Pragser Wildsee, near Toblach, to Belluno, Prags can be accessed by bus, and Belluno has both train and bus services. This is the high route in the Dolomites, and also the easiest. It gets slightly more difficult as it goes south, but the section which might present difficulties is the descent from Schiara. About 10–15 days are required to complete the full route, a typical day on the route might involve about seven hours walking, with ascents and descents of about 800 metres. It can be attempted during the period July to September, when the route should be free of snow. The route is signposted by dark blue triangles with a number one. The following maps cover the route, martino Kompass Wanderkarten Maps map number 55 Cortina d Ampezzo map number 57 Bruneck Toblach Prags map number 77 Alpi Bellunesi Kompass and Tabacco maps are readily available in the Dolomites. Camping is forbidden along the route, but there is accommodation available in mountain refuges. There are refuges all along the route, during August advance booking is essential. The Alta Via 1 passes by several Via Ferrata, but none are incorporated in the route, the highest point on the route is Monte Lagazuoi at 2,750 metres. There is a refuge on Monte Lagazuoi which has a restaurant. The route from Monte Lagazuoi descends to Falzarego Pass and then continues south, there is a cable car from the Refugio Lagazuoi to the Falzarego Pass, but a better way to descend would be through the Via Ferrata Lagazuoi Tunnels. This is a World War I tunnel which runs down through the mountain and it is also possible to descend via the Kaiserjaeger Trail and the Martini Ledge. This route passes a number of relics of the fighting took place here during World War I. The area around Monte Lagazuoi and 5 Torri is a World War I open-air museum, there are a number of other high-level routes in the Dolomites, including the Alta Via 2, which runs from Brixen to Feltre. 1, in description of this trek Organized Trailrunning and Trekking Tours on the Alta Via 1 Altavia of the Dolomites n.1 on OpenStreetMap
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Sella (Dolomites)
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The Sella group is a plateau-shaped massif in the Dolomites mountains of northern Italy. The Sella lies north of the Marmolada and to the east of the Langkofel, the highest peak is Piz Boè at 3,151 m above sea level. The Sella lies between the four Ladin valleys of Badia, Gherdëina, Fascia, and Fodom and is divided between the provinces of South Tyrol, Trentino and Belluno. It can be driven around by car crossing the Campolongo Pass, Pordoi Pass, Sella Pass, in winter it is possible to ski around the entire massif by using the Sella Ronda ski lift carousel. Also each winter the alpine touring ski Sellaronda Skimarathon race is held, the same trails can be mastered by Mountain bike during the summer. During winter the summit is the point for many alpine ski tours, of which the most famous are the descent through the Val Mesdì. Each year the course of the annual single-day seven mountain passes crossing Maratona dles Dolomites Bicycle Race goes around the Sella group, 360-degree panorama of the Sella Group, Marmolada and Fedaia lake 360-degree panorama of the Sella Group from Cima Rocca
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Marmolada
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Marmolada is a mountain in northeastern Italy and the highest mountain of the Dolomites. It lies between the borders of Trentino and Veneto, the mountain is located about 100 kilometres north-northwest of Venice, from which it can be seen on a clear day. It consists of a ridge running west to east, towards the south it breaks suddenly into sheer cliffs, forming a rock face several kilometres long. On the north there is a comparatively flat glacier, the only large glacier in the Dolomites. The ridge is composed of several summits, decreasing in altitude from west to east, Punta Penia, Punta Rocca, Punta Ombretta, Monte Serauta, an aerial tramway goes to the top of Punta Rocca. During the ski season the Marmoladas main ski run is opened for skiers and snowboarders alike, paul Grohmann made the first ascent in 1864, along the north route. The south face was climbed for the first time in 1901 by Beatrice Tomasson, Michele Bettega, until the end of World War I the border between Austria-Hungary and Italy ran over Marmolada, so it formed part of the front line during that conflict. Austro-Hungarian soldiers were quartered in deep tunnels bored into the northern faces glacier and it was also the site of fierce mine warfare on the Italian Front. As glaciers retreat, soldiers remains and belongings are occasionally discovered, white Friday List of Italian regions by highest point Computer generated summit panoramas North South Index Marmolada on Hribi. net Description of via ferrata on the Western ridge
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Tofane
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Tofane is a mountain group in the Dolomites of northern Italy, west of Cortina dAmpezzo in the province of Belluno, Veneto. Most of the Tofane lies within Parco naturale delle Dolomiti dAmpezzo, the highest peaks of the Tofane group are Tofana di Mezzo, Tofana di Dentro, and Tofana di Rozes. Tofana di Mezzo is the third highest peak in the Dolomites, after Marmolada, all three peaks were first climbed 154 years ago by Paul Grohmann along with local mountain guides, in 1863,1864 and 1865. The Dolomites were formed during the Cretaceous Period, approximately 60 million years ago, the Tofane is largely formed from the Upper Triassic rock Dolomia principale. The strata are perceptibly folded, and the mountains are formed by wind, rain. A cable lift system goes from Cortina almost to the top of Tofane di Mezzo, there is only a short walk from the top cable car to the summit. Alternatively the via ferratas VF Punta Anna and VF Gianna Aglio can be used to reach Tofane di Mezzo, some of the cabins in the Tofane are the Rifugio Angelo Dibona, the Rifugio Giussani, the Rifugio Duca dAosta, and the Rifugio Pomedes. During the First World War, the Tofane was a battlefield of the Italian Front for clashes between the Italian and Austrian forces, the front lines went through the mountains. At the 1956 Winter Olympics, Mount Tofane hosted five of the six alpine skiing events and it regularly hosts womens speed events on the World Cup circuit
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Langkofel Group
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The Langkofel Group is a massif in the Dolomites. It separates Gröden and the Fassa valley, as well as the Sella massif, northwest of the Langkofel is the Seiser Alm. The highest point in the range is the eponymous Langkofel with a height of 3,181 metres, taken together, the summits of the Langkofel form an arc which is only open towards the northwest. Within this arc there is one small mountain, the Langkofelkarspitze. The region was formed in the early Triassic period as a reef in a shallow tropical sea. Hard limestone was able to form on the outside of the reef and this left a garland of mountains which, in a clockwise direction, are the Langkofel, Langkofeleck, Fünffingerspitze, Grohmannspitze, Innerkoflerturm, Zahnkofel and Plattkofel. From there both the Langkofel, as well as the Plattkofel may be circled on hiking trails, the Plattkofel may be reached from the Langkofelkar on the klettersteig route known as the Oskar Schuster Steig and from the Plattkofel Hut over the steep western flank. Between the Langkofel and the Sellajoch is the area of known as the Rocky Town. In winter there are ski areas at the foot of the Langkofel Group, the famous Sella Ronda, a circuit of the Sella Group on ski pistes both clockwise and anticlockwise, also runs over these pistes
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Pala (Dolomites)
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The Pala group is a mountain range in the Dolomites, in the eastern Trentino and part of the province of Belluno, northern Italy. They cover an area of c.240 km² between the Primiero, Valle del Biois and Agordino and they include a large plateau, spanning for some 50 km² between 2,500 and 2,800 m, an empty rocky extent. Geologically, they are composed of dolostone. Vezzana,3,192 m Cimon della Pala,3,184 m Cima dei Bureloni,3,130 m Cima di Focobon,3,054 m Pala di San Martino,2,982 m Fradusta,2,939 m Mulaz,2,906 m Sass Màor,2,812 m. Cima Madonna,2,752 m Rosetta,2,743 m Favaretto, pale di San Martino, il paese delle meraviglie di roccia
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This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Dolomites, The". Encyclopædia Britannica. 8 (11th ed.). Cambridge University Press. p. 394.
