|
Karancs Mountain
Karancs ( sk, Karanč) is the highest peak in the Karancs Hills with an elevation of . It lies on the Hungarian-Slovak border. In Hungary, the mountain forms part of the Karancs-Medves Protected Landscape Area, while in Slovakia it is included in the Cerová vrchovina Protected Landscape Area. The name ''Karancs'' may be derived from the mountain's often dark green (almost black) colour. In Pecheneg and the other Middle Turkic Middle Turkic (''Türki'' or ''Türkçe'') refers to a phase in the development of the Turkic language family, covering much of the Middle Ages (c. 900–1500 CE). In particular the term is used by linguists to refer to a group of Karluk and Og ... languages, the word ''kara'' meant 'black', or from qurunçï 'sooty, charred felt'. Another possible etymology is that the word was formed from the toponymic base ''karant'', derived from the Proto-Celtic *''karn-'' and ultimately from the Proto-Indo-European *''ḱerh₂-'' meaning "highest part of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pecheneg Language
Pecheneg is an extinct Turkic language spoken by the Pechenegs in Eastern Europe (parts of Southern Ukraine, Southern Russia, Moldova, Romania and Hungary) in the 7th–12th centuries. However, names in this language (Beke, Wochun, Lechk, etc) are reported from Hatvan until 1290. Byzantine princess Anna Komnene asserts that the Pechenegs and Cumans spoke the same language. It was most likely a member of the Oghuz branch of the Turkic family,Баскаков, Н. А. Тюркские языки, Москва 1960, с. 126-131. but poor documentation and the absence of any descendant languages have prevented linguists from making an accurate classification; most experts would be fairly confident in placing it among the Oghuz languages, but would refuse to classify it further, though it is placed in the Kipchak language family in Glottolog and in the Kipchak–Cuman language family in Linguist List The LINGUIST List is a major online resource for the academic field of linguist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Turkic
Middle Turkic (''Türki'' or ''Türkçe'') refers to a phase in the development of the Turkic language family, covering much of the Middle Ages (c. 900–1500 CE). In particular the term is used by linguists to refer to a group of Karluk and Oghuz and related languages spoken during this period in Central Asia, Iran Iran, officially the Islamic Republic of Iran, and also called Persia, is a country located in Western Asia. It is bordered by Iraq and Turkey to the west, by Azerbaijan and Armenia to the northwest, by the Caspian Sea and Turkmeni ..., and other parts of the Middle East controlled by the Seljuk Turks. Classification Middle Turkic can be divided into eastern and western branches. Eastern Middle Turkic consists of Karakhanid language, Karakhanid (also called Khaqani Turkic), a literary language which was spoken in Kashgar, Balasaghun and other cities along the Silk Road and its later descendents such as Khorezmian language (Turkic), Khorezmian and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laccolith
A laccolith is a body of intrusive rock with a dome-shaped upper surface and a level base, fed by a conduit from below. A laccolith forms when magma (molten rock) rising through the Earth's crust begins to spread out horizontally, prying apart the host rock strata. The pressure of the magma is high enough that the overlying strata are forced upward, giving the laccolith its dome-like form. Over time, erosion can expose the solidified laccolith, which is typically more resistant to weathering than the host rock. The exposed laccolith then forms a hill or mountain. The Henry Mountains of Utah, US, are an example of a mountain range composed of exposed laccoliths. It was here that geologist Grove Karl Gilbert carried out pioneering field work on this type of intrusion. Laccolith mountains have since been identified in many other parts of the world. Description A laccolith is a type of igneous intrusion, formed when magma forces its way upwards through the Earth's crust b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proto-Indo-European
Proto-Indo-European (PIE) is the reconstructed common ancestor of the Indo-European language family. Its proposed features have been derived by linguistic reconstruction from documented Indo-European languages. No direct record of Proto-Indo-European exists. Far more work has gone into reconstructing PIE than any other proto-language, and it is the best understood of all proto-languages of its age. The majority of linguistic work during the 19th century was devoted to the reconstruction of PIE or its daughter languages, and many of the modern techniques of linguistic reconstruction (such as the comparative method) were developed as a result. PIE is hypothesized to have been spoken as a single language from 4500 BC to 2500 BC during the Late Neolithic to Early Bronze Age, though estimates vary by more than a thousand years. According to the prevailing Kurgan hypothesis, the original homeland of the Proto-Indo-Europeans may have been in the Pontic–Caspian steppe of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proto-Celtic
Proto-Celtic, or Common Celtic, is the ancestral proto-language of all known Celtic languages, and a descendant of Proto-Indo-European. It is not attested in writing but has been partly Linguistic reconstruction, reconstructed through the comparative method. Proto-Celtic is generally thought to have been spoken between 1300 and 800 BC, after which it began to split into different languages. Proto-Celtic is often associated with the Urnfield culture and particularly with the Hallstatt culture. Celtic languages share common features with Italic languages that are not found in other branches of Indo-European, suggesting the possibility of an earlier Italo-Celtic linguistic unity. Proto-Celtic is currently being reconstructed through the comparative method by relying on later Celtic languages. Though Continental Celtic presents much substantiation for Proto-Celtic phonology, and some for its morphology (linguistics), morphology, recorded material is too scanty to allow a secure rec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kara
Kara or KARA may refer to: Geography Localities * Kara, Chad, a sub-prefecture * Kára, Hungary, a village * Kara, Uttar Pradesh, India, a township * Kara, Iran, a village in Lorestan Province * Kara, Republic of Dagestan, a rural locality in Dagestan, Russia * Kara, Sardauna, a village in Sardauna, Nigeria * Kara, Bougainville, a town on Bougainville Island in Papua New Guinea * Kara, Togo, a city in northern Togo ** Kara Region ** Roman Catholic Diocese of Kara, Togo * Gaya confederacy or Kara, a former confederation in the southern Korean peninsula * Kara crater, a meteorite crater in northern Russia Rivers, Seas * Kara (river), a river in northern Russia, flowing into the Kara Sea * Kara River (other), other rivers named Kara * Kara Lake, Bolivia * Kara Sea, a sea in the Arctic Ocean * Kara Strait, a strait in Russia People * Kara (name), a surname and given name, and a list of people with the name * Kara people, an ethnic group in Sudan they exceed 100,000 mem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pecheneg
The Pechenegs () or Patzinaks tr, Peçenek(ler), Middle Turkic: , ro, Pecenegi, russian: Печенег(и), uk, Печеніг(и), hu, Besenyő(k), gr, Πατζινάκοι, Πετσενέγοι, Πατζινακίται, ka, პაჭანიკი, bg, печенеги, pechenegi, bg, печенези, ; sh-Latn-Cyrl, Pečenezi, separator=/, Печенези, la, Pacinacae, Bisseni were a semi-nomadic Turkic ethnic people from Central Asia who spoke the Pecheneg language which belonged to the Oghuz branch of the Turkic language family. Ethnonym The Pechenegs were mentioned as ''Bjnak'', ''Bjanak'' or ''Bajanak'' in medieval Arabic and Persian texts, as ''Be-ča-nag'' in Classical Tibetan documents, and as ''Pačanak-i'' in works written in Georgian. Anna Komnene and other Byzantine authors referred to them as ''Patzinakoi'' or ''Patzinakitai''. In medieval Latin texts, the Pechenegs were referred to as ''Pizenaci'', ''Bisseni'' or ''Bessi''. East Slavic peo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nógrád (county)
Nógrád ( sk, Novohrad; german: Neuburg) is a village in Nógrád County, Hungary. Etymology The name comes from Slavic ''Novgrad'' ("New Castle") from which evolved Slovak language, Slovak ''Novohrad'' (with the same meaning) and Hungarian ''Nógrád''. 1138/1329 ''civitas Naugrad'', around 1200 ''castrum Nougrad'', 1217 ''castrum de Nevgrad''. The village (1405 ''villa Newgrad'') and the county was named after the castle. References External links Street map Populated places in Nógrád County {{Nograd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerová Vrchovina Protected Landscape Area
Cerová vrchovina Protected Landscape Area ( sk, Chránená krajinná oblasť Cerová vrchovina) is one of the 14 protected landscape areas in Slovakia. The Landscape Area is situated in the Cerová vrchovina Mountains, part of the Western Carpathians, in southern Slovakia. It is situated in the Rimavská Sobota, Poltár and Lučenec districts and ends at the Slovak- Hungary borders in the east. The area protects 167.71 km2 of the mountains, and it excludes all urban areas, except for the villages of Hajnáčka and Šiatorská Bukovinka. History The Protected Landscape Area was established on 10 October 1989. The law was amended on 3 September 2001. There were national nature reserves in the area before the Protected Landscape Area was created, for example Šomoška (declared in 1954) and Ragáč (1964). Geography The highest hills are Karanč / Karancs Karancs ( sk, Karanč) is the highest peak in the Karancs Hills with an elevation of . It lies on the Hungarian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
