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Karancs Hills
The Karancs Hills ( sk, Mučínska vrchovina) are a range of hills on the Hungarian-Slovakian border. The highest peak is the Karancs at above sea level.Adrian Phillips and Jo Scotchmer, Hungary (Bradt Travel Guide Hungary), 2010 References

Mountain ranges of Hungary Mountain ranges of the Western Carpathians {{Hungary-geo-stub ...
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Ragyolc Látképe
Radzovce ( hu, Ragyolc) is a village and municipality in the Lučenec District Lučenec District (''okres Lučenec'') is a district in the Banská Bystrica Region of south-central Slovakia. Until 1918, most of the district belong to the Novohrad county, with a small area around the villages of Šíd, Čamovce and Šurice ... in the Banská Bystrica Region of Slovakia. The zip code of the village is 98558. The population nationality consist of 80% Hungarian and 20% Slovak. External links * *http://www.statistics.sk/mosmis/eng/run.html Villages and municipalities in Lučenec District Municipalities in Slovakia where Hungarian is an official language {{BanskáBystrica-geo-stub ...
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Karancs
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 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 the body, horn", thus "tip, peak". Karancs is a laccolith formed through volcanic activity in the Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist ...
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Mountain Ranges Of Hungary
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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