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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] |
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] |
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 o ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kutelo
Kutelo ( ) is a summit in the Pirin mountain range, southwestern Bulgaria. With a height of 2,908 m it is the second highest peak in Pirin after Vihren (2,914 m), and the third one in Bulgaria, behind Musala (2,925 m) in Rila and Vihren. Kutelo is a double peak with a small saddle between the two parts, the lower being only one meter below the higher one, at 2,907 m. Seen from the town of Bansko it appears higher than Vihren. Like Vihren, which towers to the south, Kutelo is built up of marble but its slopes though sheer are not so rocky and it is not very difficult to climb. On the north-eastern slopes there are alpine climbing tracks of category II "b". The Premkata saddle is situated to the south and leads to Vihren while to the north is the narrow karst edge Koncheto which links Kutelo to the summit of Banski Suhodol. There are no marked tracks to the summit of Kutelo, but on the slanting western slope among the rocks is nestled the track between the Vihren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banski Suhodol
Banski Suhodol ( bg, Бански Суходол ) is a peak in the Pirin mountain, south-western Bulgaria. It is located in the northern part of Pirin on the main ridge. Its height is 2,884 m which ranks it on third place in Pirin after Vihren (2,914 m) and Kutelo (2,908 m). To the south-east of Banski Suhodol on the main ridge is located the summit of Kutelo and the two peaks are linked by the Koncheto ridge — a dizzy karst ridge which on some places is only 70 cm wide. On the main ridge to the north-west is situated a nameless peak from which to the north-east deviated the secondary karst ridge Koteshki Chal. From there the main ridge runs in west-northwest direction to the nearby Bayuvi Dupki peak (2,820 m). The north-eastern slope of Banski Suhodol is a vertical 300-meter marble wall that lowers down to the cirque of the same name. There are a lot of places in the cirque where the snow remains the whole year, several karst caves have been discov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koncheto
Koncheto ( , ) is a name given to a knife-edge ridge in the Pirin Mountains in Bulgaria, at an elevation of approximately 2,810 metres, between the peaks Banski Suhodol (2,884 meters) and Kutelo (2,908 metres). There are steep slopes on either side: the northwestern side is almost vertical and 300–400 metres deep, while the southwestern side is less steep (approximately 30 degrees) but deeper (800 metres). There is a steel cable stretched along the top of the ridge to help hikers across. It is said that some less experienced hikers go through Koncheto by saddling the ridge edge like a horse and slowly advancing, hence its name. It is not recommended for hikers with acrophobia Acrophobia is an extreme or irrational fear or phobia of heights, especially when one is not particularly high up. It belongs to a category of specific phobias, called space and motion discomfort, that share both similar causes and options fo .... References Pirin Landforms of Blagoevgrad Pro ... [...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, althou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maja Jezerce
Maja can refer to: Places * Maja, Croatia, a village * Maja, Banten, a subdistrict in Lebak Regency, Banten, Indonesia ** Maja railway station * Maja, West Java, a subdistrict in Majalengka Regency, West Java, Indonesia * Maja River, a tributary of the Angke River, Jakarta, Indonesia * Maja (peak), a mountain peak in Kosovo * Maja (river), a river in Romania * Mája, the Hungarian name for Maia village, Bereni Commune, Mureș County, Romania * 66 Maja, a main-belt asteroid People * Maja (given name), a feminine given name * Charles Maja (1966–2020), South African actor * Josh Maja (born 1998), English footballer * Otto Maja (born 1987), Finnish street artist * Maja, the feminine form of majo, a low-class Spaniard of the 18th and 19th century Animals * Maja (boa constrictor), a species in the Cuban cactus scrub * ''Maja'' (crab), a genus of crabs in the family Majidae See also * Maia (other) * ''La maja desnuda'', a painting by Spanish artist Francisco Goya * '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albania
Albania ( ; sq, Shqipëri or ), or , also or . officially the Republic of Albania ( sq, Republika e Shqipërisë), is a country in Southeastern Europe. It is located on the Adriatic and Ionian Seas within the Mediterranean Sea and shares land borders with Montenegro to the northwest, Kosovo to the northeast, North Macedonia to the east and Greece to the south. Tirana is its capital and largest city, followed by Durrës, Vlorë, and Shkodër. Albania displays varied climatic, geological, hydrological, and morphological conditions, defined in an area of . It possesses significant diversity with the landscape ranging from the snow-capped mountains in the Albanian Alps as well as the Korab, Skanderbeg, Pindus and Ceraunian Mountains to the hot and sunny coasts of the Albanian Adriatic and Ionian Sea along the Mediterranean Sea. Albania has been inhabited by different civilisations over time, such as the Illyrians, Thracians, Greeks, Romans, Byzantines, Veneti ... [...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] |
Gran Sasso
Gran Sasso d'Italia (; ) is a massif in the Apennine Mountains of Italy. Its highest peak, Corno Grande (2,912 metres), is the highest mountain in the Apennines, and the second-highest mountain in Italy outside the Alps. The mountain lies within Gran Sasso e Monti della Laga National Park. Geography The three main summits of the Gran Sasso are Corno Grande, which at is the highest peak in the Apennines, nearby ''Corno Piccolo'', and ''Pizzo d'Intermesoli'', which is separated from the other two peaks by Val Maone, a deep valley. Corno Grande and Corno Piccolo's ash coloration come from their limestone and dolomite composition. The peaks are snow-covered for much of the year though the snow cover appears to be less each decade. Corno Piccolo is referred to as, "The Sleeping Giant". This is due to the appearance of a profile of a reclined face. This view of Corno Piccolo is evident when viewing the mountain from Pietracamela, a small town near Prati di Tivo, on the north side ... [...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 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] |
