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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] |
Europe
Europe is a large peninsula conventionally considered a continent in its own right because of its great physical size and the weight of its history and traditions. Europe is also considered a Continent#Subcontinents, subcontinent of Eurasia and it is located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. Comprising the westernmost peninsulas of Eurasia, it shares the continental landmass of Afro-Eurasia with both Africa and Asia. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south and Asia to the east. Europe is commonly considered to be Boundaries between the continents of Earth#Asia and Europe, separated from Asia by the drainage divide, watershed of the Ural Mountains, the Ural (river), Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea and the waterways of the Turkish Straits. "Europe" (pp. 68–69); "Asia" (pp. 90–91): "A commonly accepted division between Asia and E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Musala
Musala ( bg, Мусала ); from Arabic language, Arabic through Ottoman Turkish language, Ottoman Turkish: from ''Musalla'', "near God" or "place for prayer" is the highest mountain, peak in the Rila, Rila Mountains, as well as in Bulgaria and the entire Balkan Peninsula, standing at . With a topographic prominence of , Musala is also the List of European ultra-prominent peaks, 6th highest peak by topographic prominence in Continental Europe, mainland Europe. Musala is also the Most isolated major summits of Europe, 3rd most topographically isolated major peak in Continental Europe. Musala is situated within the Rila National Park, which is noted for its rich Flora (plants), flora, including species such as Macedonian Pine and Bulgarian Fir in the forests on its middle slopes, and Fauna (animals), fauna; it is one of the easiest places in Europe to see the wallcreeper. All major mountain ranges of Bulgaria can be seen from the top; these include Vitosha to the northwest, Sredn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aneto 01
Aneto (''pic d'Aneto'' in French, formerly ''pic de Néthou'') is the highest mountain in the Pyrenees and in Aragon, and Spain's third-highest mountain, reaching a height of . It stands in the Spanish province of Huesca, the northernmost of the three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif. Aneto is located in the Posets-Maladeta Natural Park, in the municipality of Benasque, Huesca province, autonomous community of Aragon, Spain. It is part of the Maladeta massif and is located in the Benasque valley. It consists of Paleozoic terrain of a granitic nature and Mesozoic materials. Its northern side holds the largest glacier in the Pyrenees, covering in 2005; it is shrinking rapidly due to warming summer temperatures and decreasing winter precipitations over the 20th century – it covered 106.7 ha in 1981, and over 200 ha in the 19th century. It is estimated that it has lost more than half of its s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snezhnika Glacieret July 2012
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] |
Mount Kilimanjaro
Mount Kilimanjaro () is a dormant volcano in Tanzania. It has three volcanic cones: Kibo, Mawenzi, and Shira. It is the highest mountain in Africa and the highest free-standing mountain above sea level in the world: above sea level and about above its plateau base. It is the highest volcano in Africa and the Eastern Hemisphere. Kilimanjaro is the fourth most topographically prominent peak on Earth. It is part of Kilimanjaro National Park and is a major hiking and climbing destination. Because of its shrinking glaciers and ice fields, which are projected to disappear between 2025 and 2035, it has been the subject of many scientific studies. Toponymy The origin of the name Kilimanjaro is not known, but a number of theories exist. European explorers had adopted the name by 1860 and reported that Kilimanjaro was the mountain's Kiswahili name. The 1907 edition of ''The Nuttall Encyclopædia'' also records the name of the mountain as Kilima-Njaro. Johann Ludwig Krapf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kenya
Mount Kenya (Kikuyu: ''Kĩrĩnyaga'', Kamba, ''Ki Nyaa'') is the highest mountain in Kenya and the second-highest in Africa, after Kilimanjaro. The highest peaks of the mountain are Batian (), Nelion () and Point Lenana (). Mount Kenya is located in the former Eastern and Central provinces of Kenya; its peak is now the intersection of Meru, Embu, Laikipia, Kirinyaga, Nyeri and Tharaka Nithi counties, about south of the equator, around north-northeast of the capital Nairobi. Mount Kenya is the source of the name of the Republic of Kenya. Mount Kenya is a volcano created approximately 3 million years after the opening of the East African Rift. Before glaciation, it was high. It was covered by an ice cap for thousands of years. This has resulted in very eroded slopes and numerous valleys radiating from the peak. There are currently 11 small glaciers, which are shrinking rapidly, and may disappear by 2050. The forested slopes are an important source of water for much of Keny ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rwenzori Mountains
The Ruwenzori, also spelled Rwenzori and Rwenjura, are a range of mountains in eastern equatorial Africa, located on the border between Uganda and the Democratic Republic of the Congo. The highest peak of the Ruwenzori reaches , and the range's upper regions are permanently snow-capped and glaciated. Rivers fed by mountain streams form one of the sources of the Nile. Because of this, European explorers linked the Ruwenzori with the legendary Mountains of the Moon, claimed by the Greek scholar Ptolemy as the source of the Nile. Virunga National Park in eastern DR Congo and Rwenzori Mountains National Park in southwestern Uganda are located within the range. Geology The mountains formed about three million years ago in the late Pliocene epoch and are the result of an uplifted block of crystalline rocks including gneiss, amphibolite, granite and quartzite. The Rwenzori mountains are the highest non-volcanic, non-orogenic mountains in the world. This uplift divided the pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers In Africa
Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacial maximum 10,000 to 15,000 years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Currently, the only remaining glaciers on the continent exist on Mount Kilimanjaro, Mount Kenya, and the Rwenzori. List of glaciers Kenya (All located on the upper slopes of Mount Kenya) *Mr. Ali Cesar Glacier *Diamond Glacier *Darwin Glacier (Kenya) *Forel Glacier *Gregory Glacier *Heim Glacier *Josef Glacier *Kraph Glacier *Lewis Glacier *Northey Glacier *Tyndall Glacier Rwenzori Mountains *Speke Glacier *Elena *Stanley *Baker Tanzania All Tanzanian glaciers are located on the summit of Mount Kilimanjaro. The mountain had 16 named glaciers and three icefields in the middle of the 20th century but by the 1990s, at least 4 glaciers had disappeared and the remain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maglić (mountain)
Maglić ( sr-cyrl, Маглић, ) is transboundary mountain, on the border of Bosnia and Herzegovina and Montenegro. The highest peak is at an elevation of , and is located within Montenegro, however, its twin peak, the most visited of two, is also second highest at which makes it the highest peak of Bosnia and Herzegovina. The mountain is oriented in a northwest–southeast direction. Geography Maglić is the highest mountain in Bosnia and Herzegovina. It is bounded by the river Sutjeska to the west, the Piva to the east-southeast and the Upper Drina to the north-northeast, with Vučevo plateau () extending to the north. Foča city near the border with Montenegro is away from the Maglić massif and the nearest town is Mratinje. Karst limestone formations in the region of limestone plateau are the general geological setting in the south and southwest region. Maglić massif consists of two peaks namely, the Veliki Maglić () on the Bosnia and Herzegovina side and the Crno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantabrian Mountains
, etymology=Named after the Cantabri , photo=Cordillera Cantábrica vista desde el Castro Valnera.jpg , photo_caption=Cantabrian Mountains parallel to the Cantabrian Sea seen from Castro Valnera in an east-west direction. In the background, the Montaña Palentina (left) and the Picos de Europa (right) , country= Spain , subdivision1_type=Communities , subdivision1= , geology= Limestone , age= Carboniferous, Paleozoic, Mesozoic , orogeny= , borders_on= , area_km2= , length_km=300 , length_orientation=WE , width_km= 50 , width_orientation=NS , highest= Torre de Cerredo , elevation_m= 2648 , range_coordinates= , coordinates= , map_image=Cordillera Cantabrica.jpg , map_caption=Location of the Cantabrian Mountains in northern Spain , parent= The Cantabrian Mountains or Cantabrian Range ( es, Cordillera Cantábrica) are one of the main systems of mountain ranges in Spain. They stretch for over 300 km (180 miles) across northern Spain, from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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