|
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, althou ... [...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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 lakes and streams, a number of Pirin's lakes are located around the peak, as is Europe's southernmost glacial mass, the Snezhnika glacieret. Until 1942 Vihren was known as ''Eltepe'' (peak of storms); it was also called ''Buren'' (stormy) and ''Malnienosets'' (lightning-bringer). The UNESCO World Heritage Site Pirin National Park was originally known as the ''Vihren National Park''. Vihren is included in the 100 Tourist Sites of Bulgaria under No. 2. Geography Vihren is situated in the northern subdivision of Pirin on the mountain's main ridge between the summits of Kutelo (2,908 m) to the north-west and Hvoynati Vrah (2,635 m) to the south-east. It is connected with these two peaks via the saddles of Premkata (2,610 m) to the north and Kab ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maja Jezercë
Jezerca Peak ( sq, Maja Jezercë) is the highest peak in the Dinaric Alps, the fifth highest in Albania and the sixth highest in the Balkans, standing at above sea level. It is the 28th most prominent mountain peak in Europe, and is regarded as one of the toughest and most dangerous climbs in the Albanian Alps. Maja Jezercë is situated within the Accursed Mountains range, which is noted for several small glaciers - among the southernmost glacial masses in Europe after Snezhnika glacier (latitude of 41°46′09″ N)Grunewald, p. 129. and Banski Suhodol Glacier in Pirin mountain in Bulgaria. Apart from certain areas north of the peak, the limestone mountain massif is part of the National Parks of Theth and Valbonë Valley. It can be climbed from the north; most climbers come from Gusinje in Montenegro as well as from Theth. The summit is from the border with Montenegro, between the Valleys of Valbonë to the east and the Shala to the west. In part, the whole floor b ... [...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] |
Golemiya Kazan
Golemiya Kazan ( bg, Големия казан) is one of the two cirques that form an area called ''Kazanite'' (the Cauldrons), situated in Bulgaria's Pirin mountain range. ''Kazanite'' are located below the two highest summits Vihren (2,914 m) to the south and Kutelo (2,908 m) to the north. It is composed of two cirques, ''Malkiya Kazan'' (The Small Cauldron), which is the lower one (2,200 m) and is grassy, and ''Golemiya Kazan'' (The Big Cauldron), situated at 2,400 m and with stony slopes. The size of Golemiya Kazan is 1,200 m by 1,100 m. They were named like that because there is often fog rising from the cirques. Due to the karst in the region there are no lakes or streams in ''Kazanite''. A 450 m-high face of Vihren begins from Golemiya Kazan and at its foot a small glacier called Snezhnika is located, whose size is 80x90 m in summer, with a latitude of 41°46′09″ N it is the southernmost glacial mass in EuropeGrunewald, p. 129. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 V ... 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'', 32, 1593-1602. References ... [...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 ... [...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_date ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque Glacier
A cirque glacier is formed in a cirque, a bowl-shaped depression on the side of or near mountains. Snow and ice accumulation in corries often occurs as the result of avalanching from higher surrounding slopes. If a cirque glacier advances far enough, it may become a valley glacier. Additionally, if a valley glacier retreats enough that it is within the cirque, it becomes a cirque glacier again. In these depressions, snow persists through summer months, and becomes glacier ice. Snow may be situated on the leeward slope of a mountain, where it is sheltered from wind. Rock fall from above slopes also plays an important role in sheltering the snow and ice from sunlight. If enough rock falls onto the glacier, it may become a rock glacier. Randklufts may form beneath corrie glaciers as open space between the ice and the bedrock, where meltwater Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apennines
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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
