Glaciers Of Tanzania
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Glaciers Of Tanzania
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 rema ...
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Glacier At Summit Of Mt Kilimanjaro 001
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 only in ...
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Credner Glacier
Credner Glacier is on Mount Kilimanjaro in Tanzania, on the northwest slope of the peak and is a remnant of an icecap which once crowned the top of Mount Kilimanjaro. The glacier is situated at an elevation of between . Credner Glacier is one of the largest glaciers on the mountain and descends from the Northern Ice Field. Credner is rapidly retreating due to its high exposure point on the northwest slope of Mount Kilimanjaro. A report published in 2013 indicated that in another decade the glacier may no longer exist. File:Lava Expeditions Credner Glacier 3.jpg, Credner Glacier and recently exposed old lava in 2009 File:Lava Expeditions Credner Glacier 7.jpg, Scientist atop Credner Glacier in 2009 See also *Retreat of glaciers since 1850 *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 i ...
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Glaciers Of Africa
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 only in ...
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Mountains Of The Moon (Africa)
250px, ''Jibhel Kumri'' or Mountains of the Moon as conceived in 1819 Mountains of the Moon (Latin: ''Montes Lunae''; ar, جبل القمر, ' or ''Jibbel el Kumri'') is an ancient term referring to a legendary mountain or mountain range in east Africa at the source of the Nile River. Various identifications have been made in modern times, the Rwenzori Mountains of Uganda and the Democratic Republic of the Congo being the most celebrated. Ancient testimony People of the ancient world were long curious about the source of the Nile, especially Ancient Greek geographers. A number of expeditions up the Nile failed to find the source. Eventually, a merchant named Diogenes reported that he had traveled inland from Rhapta in East Africa for twenty-five days and had found the source of the Nile. He reported that it flowed from a group of massive mountains into a series of large lakes. He reported the natives called this range the Mountains of the Moon because of their snowcapped whiten ...
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Geography Of Africa
Africa is a continent comprising 63 political territories, representing the largest of the great southward projections from the main mass of Earth's surface. Within its regular outline, it comprises an area of , excluding adjacent islands. Its highest mountain is Mount Kilimanjaro, its largest lake is Lake Victoria. Separated from Europe by the Mediterranean Sea and from much of Asia by the Red Sea, Africa is joined to Asia at its northeast extremity by the Isthmus of Suez (which is transected by the Suez Canal), wide. For geopolitical purposes, the Sinai Peninsula of Egypt – east of the Suez Canal – is often considered part of Africa. From the most northerly point, Ras ben Sakka in Tunisia, at 37°21′ N, to the most southerly point, Cape Agulhas in South Africa, 34°51′15″ S, is a distance approximately of ; from Cap-Vert, 17°31′13″W, the westernmost point, to Ras Hafun in the Somali Puntland region, in the Horn of Africa, 51°27′52″ E, the most ...
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Rebmann Glacier
The Rebmann Glacier is an active glacier located near the summit of Mount Kilimanjaro in Tanzania. It is a small remnant of an enormous ice cap which once crowned Kilimanjaro. This ice cap has retreated significantly over the past century; between 1912 and 2000, 82 percent of the glacial ice on the mountain disappeared. Rebmann Glacier is named for German missionary and explorer Johann Rebmann, who was the first European explorer to report observations of snow and glaciers atop Kilimanjaro, in 1848. See also *Retreat of glaciers since 1850 *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 Sout ... References Glaciers of Tanzania Pangani basin {{Tanzania-glacier-stub ...
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Northern Ice Field (Mount Kilimanjaro)
The Northern Ice Field is near the summit of Mount Kilimanjaro in Tanzania, on the west slope of the peak. The Northern Ice Field and Eastern Ice Fields were connected to the Southern Ice Field and formed part of a continuous body of glacial ice atop Mount Kilimanjaro when first scientifically examined in 1912. By 1962 the Southern Ice Field separated from the Northern Ice Field and then by 1975 the Eastern Ice Field did as well. In 1912, the glaciated areas atop Mount Kilimanjaro covered ; by 2011 this had been reduced to , an 85 percent loss. At one time, ice flowing off the Northern Ice Field fed numerous glaciers, including, north to south, the Credner, Drygalski, Great Penck and Little Penck Glaciers. The Northern Ice Field is the largest body of ice remaining on Mount Kilimanjaro, with an area of , when measured in 2007. During the exceptionally cold period known as the Younger Dryas, which occurred approximately 12,800 and 11,500 years BP (between 10,800 and ...
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Little Penck Glacier
Little Penck Glacier is on Mount Kilimanjaro in Tanzania, on the west slope of the peak. Once extending from the Northern Ice Field, the glacier detached from the icefield by 1992. A sizeable but stagnant ice body remains near the 1912 historical terminal end of the glacier. The now vanished Great Penck and Uhlig Glaciers once flanked Little Penck Glacier to the north and south, respectively. See also *Retreat of glaciers since 1850 *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 Sout ... References Glaciers of Tanzania {{Tanzania-glacier-stub ...
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Great Penck Glacier
Great Penck Glacier was on Mount Kilimanjaro in Tanzania, on the west slope of the peak. Extending from the Northern Ice Field, the glacier once flowed , to an elevation of . Between the years 1962 and 1975, Great Penck Glacier separated from the Northern Icefield and disappeared. Drygalski Glacier once also existed to the north of Great Penck, while the same is true of the Little Penck Glacier, which was to the south. See also *Retreat of glaciers since 1850 *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 Sout ... References Glaciers of Tanzania {{Tanzania-glacier-stub ...
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Furtwängler Glacier
Furtwangler Glacier is located near the summit of Mount Kilimanjaro in Tanzania. The glacier is named after who, with Siegfried König, formed the fourth party to ascend to the summit of Kilimanjaro in 1912. The glacier is a small remnant of an ice cap that once crowned the summit of Kilimanjaro. Almost 85 percent of the ice cover disappeared from October 1912 to June 2011. In 2013 it was estimated that at the then-current rate, most of the ice would disappear by 2040 and "it is highly unlikely that any ice body will remain after 2060". Furtwängler Glacier is ephemeral, existing continuously only since about 1650 CE, which corresponds with very high levels in Kenya's Lake Naivasha and the beginning of the Maunder Minimum. Between measurements in 1976 and 2000, the area of this glacier was cut almost in half, from to . By 2018 the size had shrunk to . In 2022 it was thought that the glacier would cease to exist by 2023 at a rate of loss of per year. During fieldwork conducte ...
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Drygalski Glacier (Tanzania)
Drygalski Glacier was on Mount Kilimanjaro in Tanzania, on the northwest slope of the peak. The glacier terminus once extended to an elevation of with an origination point near the summit of Mount Kilimanjaro and was fed by the Northern Ice Field. The Great Penck Glacier once flanked Drygalski Glacier to the south and until recently, the Credner Glacier did as well to the north. Drygalski Glacier is named for German geographer Erich von Drygalski. See also *Retreat of glaciers since 1850 *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 Sout ... References Glaciers of Tanzania {{Tanzania-glacier-stub ...
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