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Debeli Namet
Debeli Namet is a small glacier below Mount Šljeme () in the Durmitor massif, Montenegro. Geography This glacier exists well below the true snowline and is sustained by avalanching snow. Results of recent investigations on the Debeli Namet glacier have been published by a British scientist (Hughes 2007). The Debeli Namet glacier is not quite the southernmost glacier in Europe, as this status currently goes to the Snezhnika glacier (latitude of 41°46′09″ N) followed by Banski Suhodol Glacier also in Pirin mountain in Bulgaria and the Calderone Glacier in Italy.Hughes, P.D. (2007) Recent behaviour of the Debeli Namet glacier, Durmitor, Montenegro. ''Earth Surface Processes and Landforms ''Earth Surface Processes and Landforms'' is a peer-reviewed scientific journal published by John Wiley & Sons on behalf of the British Society for Geomorphology. It covers geomorphology and more in general all aspects of Earth sciences dealing w ...'', 32, 1593-1602. References {{Mon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durmitor
Durmitor ( Montenegrin: Дурмитор, or ) is a massif located in northwestern Montenegro. It is part of the Dinaric Alps. Its highest peak, Bobotov Kuk, reaches a height of . The massif is limited by the Tara River Canyon on the north, the Piva River Canyon on the west, and by the Komarnica River Canyon on the south. To the east, the Durmitor opens to a high plateau, called ''Jezerska površ'' (Plateau of Lakes). The Sinjavina mountain is located to the east of the ''Jezerska površ'' plateau. The Durmitor is for the most part located in the Žabljak municipality. The massif gives its name to the national park that comprises it. Durmitor National Park was founded in 1952, and designated as a World Heritage Site in 1980. Peaks The massif has 48 peaks above . Highest peaks are: * Bobotov kuk * Bezimeni vrh (Nameless Peak) * Šljeme * Istočni vrh Šljemena (East Peak of Sljeme) * Soa / Đevojka * Milošev tok * Bandijerna * Rbatina * Lučin vrh * Prutaš * Minin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montenegro
) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_year = 2011 , religion = , religion_year = 2011 , demonym = Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Milo Đukanović , leader_title2 = Prime Minister , leader_name2 = Dritan Abazović (acting) , leader_title3 = Speaker , leader_name3 = Danijela Đurović , legislature = Skupština , sovereignty_type = Establishment history , established_event1 = Principality of Duklja , established_date1 ... [...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#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, 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 lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southernmost Glacial Mass In Europe
The southernmost persistent glacial masses in Europe are mainly small glaciers, glacierets, and perennial firn fields and patches, located in the highest mountains of the three big southern European peninsulas - the Balkan, the Apennine, and the Iberian, the southernmost ranges of the Alps and the glaciers on the european northwestern slopes of the Greater Caucasus mountains in Russia. There are summer lasting snow patches in Sierra Nevada (Corral de la Veleta glacier at 37°03′24″ disappeared completely for a first time in 1913), in Mount Olympus (40°05′08″) (Kazania cirque), in Mount Korab (41°47′28″), in Rila Mountain (the cirque of the Seven Rila Lakes, Musala and Malyovitsa (42°10′25″) ridges), in Picos de Europa (43°11′51″) in the Cantabrian Mountains, in Mount Maglić (43°16′52″) and others. However, none of them have both persistency and indications of dynamic motion. In southern direction, some 4000 km away, are the glaciers in Africa i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snezhnika
Snezhnika ( bg, Снежника 'the snow patch') is a glacieret in the Pirin Mountains of Bulgaria, a remnant of the former Vihren Glacier.Grunewald, p. 129. The glacieret lies at an elevation between and in the deep Golemiya Kazan cirque at the steep northern foot of Vihren (), Pirin's highest summit. Due to the relatively easy access and its location along a popular hiking trail, Snezhnika is Bulgaria's most famous glacieret. Snezhnika has an average area of and in 2006 it had a volume of . Snezhnika's size varies in length from 70 to 100 metres (west to east) and in width from 40 to 90 metres (north to south). Its firn is 8–11 m thick at the base and its snow cover, which is mostly fed by avalanche snow, can be as deep as 20 metres in March and April. Snezhnika's latitude of 41°46′09″ N makes it the southernmost glacial mass in Europe;http://geoproblems.eu/wp-content/uploads/2016/01/2013_12/7_gachev.pdf the nearby Banski Suhodol Glacier below Koncheto, although ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banski Suhodol Glacier
The Banski Suhodol Glacier ( bg, Ледника в Бански Суходол, ''Lednika v Banski Suhodol'') is a small glacier (glacieret) in the Pirin Mountains of Bulgaria. It lies below the Kutelo peak (2908 m.) in the upper Banski Suhodol Valley ( bg, Бански Суходол). Geography The glacier is on the northern slope of the Kutelo summit and is shaded from the east by the Koncheto ridge. After the nearby Snezhnika glacier (latitude of 41°46′09″ N) Banski Suhodol glacier is the southernmost in Europe, followed by three small glaciers below the Maja Jezerce summit in northern Albania, the Calderone glacier in the Gran Sasso mountain in Italy, and Debeli Namet glacier in Montenegro. Together with the nearby Snezhnika glacieret below Vihren Vihren ( ) is the highest peak of Bulgaria's Pirin Mountains. Reaching , it is Bulgaria's second and the Balkans' third highest, after Musala and Mount Olympus. Although due to the karst topography Vihren is deprived of la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landform Analysis
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pirin
, photo=Pirin-mountains-Bansko.jpg , photo_caption=Pirin scenery in winter , country= Bulgaria, , parent= , geology= granite, gneiss, marble, limestone , area_km2=2585 , range_coordinates = , length_km=80 , length_orientation= north-south , width_km=40 , width_orientation= north-south , highest= Vihren , elevation_m=2915 , coordinates = , map_image=Bulgaria Pirin mountain geographic map bg.svg The Pirin Mountains ( bg, Пирин ) are a mountain range in southwestern Bulgaria, with Vihren at an altitude of 2,914 m being the highest peak. The range extends about 80 km from the north-west to the south-east and is about 40 km wide, spanning a territory of . To the north Pirin is separated from Bulgaria's highest mountain range, the Rila Mountain, by the Predel saddle, while to the south it reaches the Slavyanka Mountain. To the west is located the valley of the river Struma and to the east the valley of the river Mesta separates it from the Rh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bulgaria
Bulgaria (; bg, България, Bǎlgariya), officially the Republic of Bulgaria,, ) is a country in Southeast Europe. It is situated on the eastern flank of the Balkans, and is bordered by Romania to the north, Serbia and North Macedonia to the west, Greece and Turkey to the south, and the Black Sea to the east. Bulgaria covers a territory of , and is the sixteenth-largest country in Europe. Sofia is the nation's capital and largest city; other major cities are Plovdiv, Varna and Burgas. One of the earliest societies in the lands of modern-day Bulgaria was the Neolithic Karanovo culture, which dates back to 6,500 BC. In the 6th to 3rd century BC the region was a battleground for ancient Thracians, Persians, Celts and Macedonians; stability came when the Roman Empire conquered the region in AD 45. After the Roman state splintered, tribal invasions in the region resumed. Around the 6th century, these territories were settled by the early Slavs. The Bulgars, led by Asp ... [...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 to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earth Surface Processes And Landforms
''Earth Surface Processes and Landforms'' is a peer-reviewed scientific journal published by John Wiley & Sons on behalf of the British Society for Geomorphology. It covers geomorphology and more in general all aspects of Earth sciences dealing with the Earth surface. The journal was established in 1976 as ''Earth Surface Processes'', obtaining its current name in 1981. The journal primarily publishes original research papers. It also publishes ''Earth Surface Exchanges'' which include commentaries on issues of particular geomorphological interest, discussions of published papers, shorter journal articles suitable for rapid publication, and commissioned reviews on key aspects of geomorphological science. Foci include the physical geography of rivers, valleys, glaciers, mountains, hills, slopes, coasts, deserts, and estuary environments, along with research into Holocene, Pleistocene, or Quaternary science. The editor-in-chief is Stuart Lane (University of Lausanne). Abstracting and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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