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Apennine Mountains
The Apennines or Apennine Mountains (; grc-gre, links=no, Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; la, Appenninus or – a singular with plural meaning;''Apenninus'' (Greek or ) has the form of an adjective, which would be segmented ''Apenn-inus'', often used with nouns such as ("mountain") or Greek (), but ''Apenninus'' is just as often used alone as a noun. The ancient Greeks and Romans typically but not always used "mountain" in the singular to mean one or a range; thus, "the Apennine mountain" refers to the entire chain and is translated "the Apennine mountains". The ending can vary also by gender depending on the noun modified. The Italian singular refers to one of the constituent chains rather than to a single mountain, and the Italian plural refers to multiple chains rather than to multiple mountains. it, Appennini ) are a mountain range consisting of parallel smaller chains extending along the length of peninsular Italy. In the northwest the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corno Grande
Corno Grande ( Italian for "great horn") is the highest point in the Apennine Mountains, situated in Abruzzo, central Italy. Part of the Gran Sasso massif, it is the highest peak of the Italian Peninsula at . It is the highest peak in mainland Italy outside of the Alps, and the second highest in the entire country outside the Alps, after Mount Etna in Sicily. It has significant vertical relief on the north side, though its south side is less elevated than the adjacent Campo Imperatore plateau. The northern corrie of Corno Grande holds one of the southernmost glaciers in Europe, the Calderone glacier.Grunewald, p. 129.Gachev et al. (2009), p. 16. The first recorded ascent of Corno Grande was made in 1573 by the Bolognese captain Francesco De Marchi alongside Francesco Di Domenico. The usual route of ascent is via the western ridge, although a number of other routes exist, including one that ascends the southern face. See also * List of European ultra-prominent peaks * Li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of National Parks Of Italy
The national parks of Italy are Nature reserve, protected natural areas terrestrial, marine, fluvial or lacustrine, which contain one or more intact ecosystems (or only partially altered by Anthropization, anthropic interventions) and/or one or more physical, Geology, geological, Geomorphology, geomorphological, Biology, biological formations of national and international interest, for naturalistic, scientific, cultural, aesthetic, educational or recreational values, such as to justify the intervention of the State for their conservation. There are 25 Italian national parks registered on the Official List of Protected Natural Areas (EUAP), and together cover an area of over , which correspond to approximately 5.3% of the Italian national territory. The parks are managed by the Ministry of the Environment (Italy), Ministry of the Environment based in Rome ( it, Ministero dell'Ambiente).. List of Italian national parks Parks established before the World War II Parks estab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karl Brugmann
Karl Brugmann (16 March 1849 – 29 June 1919) was a German linguist. He is noted for his work in Indo-European linguistics. Biography He was educated at the universities of Halle and Leipzig. He taught at the gymnasium at Wiesbaden and at Leipzig, and in 1872-77 was assistant at the Russian Institute of Classical Philology at the latter. In 1877 he was lecturer at the University of Leipzig, and in 1882 became professor of comparative philology there. In 1884 he took the same position at the University of Freiburg, but returned to Leipzig in 1887 as successor to Georg Curtius; for the rest of his professional life (until 1919), Brugmann was professor of Sanskrit and comparative linguistics there. As a young man, Brugmann sided with the emerging Neogrammarian school, which asserted the inviolability of phonetic laws (Brugmann's law) and adhered to a strict research methodology. As well as in laying stress on the observation of phonetic laws and their operation, it emphasized the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ernst Windisch
Ernst Wilhelm Oskar Windisch (4 September 1844, Dresden30 October 1918, Leipzig) was a German classical philologist and comparative linguist who specialised in Sanskrit, Celtic and Indo-European studies. In his student days at the University of Leipzig, he became friends with Friedrich Nietzsche. One of his teachers was Friedrich Wilhelm Ritschl. In 1867 he obtained his PhD in classical philology, afterwards teaching at the ''Thomasschule'' of Leipzig (1867–1870). In the meantime, he completed his habilitation in Sanskrit and comparative linguistics at the university (1869). In 1870–71 he worked as a staff member of the India Office Library in London. Later on, he became a professor of comparative linguistics at Heidelberg University (1872) and the University of Strasbourg (1875). In 1877 he returned to his ''alma mater'' in Leipzig as a professor of Sanskrit and director of the Indo-Europeanist institute. In the academic year of 1895/96, he served as rector. Among his stu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labialized Velar Consonant
A labialized velar or labiovelar is a velar consonant that is labialized, with a -like secondary articulation. Common examples are , which are pronounced like a , with rounded lips, such as the labialized voiceless velar plosive and labialized voiced velar plosive . Such sounds occur across Africa and the Americas, in the Caucasus, etc. Labialized velar approximants The most common labiovelar consonant is the voiced approximant . It is normally a labialized velar, as is its vocalic cousin . (Labialization is called rounding in vowels, and a velar place is called back.) and its voiceless equivalent are the only labialized velars with dedicated IPA symbols: * 1 - In dialects that distinguish between ''which'' and ''witch''. The voiceless approximant is traditionally called a "voiceless labial–velar fricative", but true doubly articulated fricatives are not known to be used in any language, as they are quite difficult to pronounce and even more difficult to distinguish. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Irish
Old Irish, also called Old Gaelic ( sga, Goídelc, Ogham script: ᚌᚑᚔᚇᚓᚂᚉ; ga, Sean-Ghaeilge; gd, Seann-Ghàidhlig; gv, Shenn Yernish or ), is the oldest form of the Goidelic/Gaelic language for which there are extensive written texts. It was used from 600 to 900. The main contemporary texts are dated 700–850; by 900 the language had already transitioned into early Middle Irish. Some Old Irish texts date from the 10th century, although these are presumably copies of texts written at an earlier time. Old Irish is thus forebear to Modern Irish, Manx, and Scottish Gaelic. Old Irish is known for having a particularly complex system of morphology and especially of allomorphy (more or less unpredictable variations in stems and suffixes in differing circumstances) as well as a complex sound system involving grammatically significant consonant mutations to the initial consonant of a word. Apparently,It is difficult to know for sure, given how little Primitiv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Celtic Language
The Celtic languages (usually , but sometimes ) are a group of related languages descended from Proto-Celtic. They form a branch of the Indo-European language family. The term "Celtic" was first used to describe this language group by Edward Lhuyd in 1707, following Paul-Yves Pezron, who made the explicit link between the Celts described by classical writers and the Welsh and Breton languages. During the 1st millennium BC, Celtic languages were spoken across much of Europe and central Anatolia. Today, they are restricted to the northwestern fringe of Europe and a few diaspora communities. There are six living languages: the four continuously living languages Breton, Irish, Scottish Gaelic and Welsh, and the two revived languages Cornish and Manx. All are minority languages in their respective countries, though there are continuing efforts at revitalisation. Welsh is an official language in Wales and Irish is an official language of Ireland and of the European Union. W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liguria
Liguria (; lij, Ligûria ; french: Ligurie) is a Regions of Italy, region of north-western Italy; its Capital city, capital is Genoa. Its territory is crossed by the Alps and the Apennine Mountains, Apennines Mountain chain, mountain range and is roughly coextensive with the former territory of the Republic of Genoa. Liguria is bordered by France (Provence-Alpes-Côte d'Azur) to the west, Piedmont to the north, and Emilia-Romagna and Tuscany to the east. It rests on the Ligurian Sea, and has a population of 1,557,533. The region is part of the Alps–Mediterranean Euroregion. Etymology The name ''Liguria'' predates Latin and is of obscure origin. The Latin adjectives (as in ) and ''Liguscus'' reveal the original root of the name, ''ligusc-'': in the Latin name -sc- was shortened to -s-, and later turned into the -r- of , according to rhotacism (sound change), rhotacism. Compare grc, λίγυς, translit=Lígus, translation=a Ligurian, a person from Liguria whence . The name de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkan Peninsula. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley. The countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro, and Slovenia. The Adriatic contains more than 1,300 islands, mostly located along the Croatian part of its eastern coast. It is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of . The Otranto Sill, an underwater ridge, is located at the border between the Adriatic and Ionian Seas. The prevailing currents flow counterclockwise from the Strait of Otranto, along the eastern coast and back to the strait along the western (Italian) coast. Tidal movements in the Adriatic are slight, although larger amplitudes are known to occur occasi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calderone Glacier
The Calderone glacier ( it, Ghiacciaio del Calderone) is a glacier located in the Apennine Mountains in Abruzzo, Italy. Found in the Gran Sasso d'Italia mountain group, it lies just beneath the Corno Grande, the highest peak in the Apennines. With the disappearance of the Corral de la Veleta glacier in the Sierra Nevada in 1913, "Il Calderone" became one of Europe's southernmost known glaciers (42°28′N, 13°33′E), being slightly to the north only compared to Snezhnika (latitude of 41°46′09″ N) and Banski Suhodol Glaciers in Pirin Mountain in Bulgaria. If present deglaciation trends continue, the Calderone may soon disappear as well. The discovery of a number of small glaciers in the Accursed Mountains in 2009 seemed to threaten Calderone's positions. Historical surface of the glacier In 1794, the Calderone had an estimated volume of over 4 million cubic metres; by 1916, the glacier’s volume had decreased to 3.3 million cubic metres, and by 1990, it had decreased t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
