"T'aa\u1E35\u00FA \u1E34w\u00E1an S\u00EDt'i"@en . . . . . "5229"^^ . . . "O glaciar Taku \u00E9 um glaciar de mar\u00E9 situado a sudeste da cidade de Juneau, no Alasca. O glaciar foi inicialmente (1883) baptizado glaciar Schultze e em 1890 glaciar Foster, mas seria a designa\u00E7\u00E3o dada ao glaciar pelos nativos tlingit, Taku, que acabaria tornando-se a designa\u00E7\u00E3o mais comum. Flui desde o campo de gelo Juneau, sendo o maior dos glaciares de descarga deste campo de gelo e um dos glaciares de mar\u00E9 mais meridionais do hemisf\u00E9rio norte. O glaciar Taku, que converge com o , apresenta um comportamento que se repete ao longo do tempo: avan\u00E7a at\u00E9 bloquear o rio, criando assim um lago, ao que se segue a rotura dram\u00E1tica da parede de gelo. O mais recente destes avan\u00E7os ocorreu em 1750. Desde 1890 o glaciar Taku avan\u00E7ou 7,5 km. \u00C9 o \u00FAnico glaciar em avan\u00E7o, entre os vinte maiores glaciares com origem no campo de gelo Juneau. A continua\u00E7\u00E3o do avan\u00E7o provocar\u00E1 mais uma vez o bloqueio do rio Taku, mas actualmente \u00E9 improv\u00E1vel que tal aconte\u00E7a. Este glaciar tem sido monitorizado anualmente desde 1946, estando documentado um avan\u00E7o m\u00E9dio de 17 metros por ano desde 1988. O avan\u00E7o \u00E9 devido a um balan\u00E7o de massa positivo, isto \u00E9, a acumula\u00E7\u00E3o de neve \u00E9 maior que a abla\u00E7\u00E3o por fus\u00E3o de gelo e neve. At\u00E9 1948 o glaciar Taku apresentava uma zona terminal da qual se desprendiam icebergues. Entre 1989 e 2005 o balan\u00E7o de massa foi negativo, mas insuficiente para parar o seu avan\u00E7o, pelo menos para j\u00E1."@pt . . . "Le glacier Taku est un glacier c\u00F4tier de l'Alaska du Sud-Est, juste au sud-est de la ville de Juneau. Le glacier fut d'abord nomm\u00E9 glacier Schultze en 1883 puis glacier Foster en 1890, mais Taku, le nom que les am\u00E9rindiens Tlingit locaux avaient pour le glacier, s'imposa. Il se trouve dans la cha\u00EEne C\u00F4ti\u00E8re (Coast Mountains) et prend naissance dans le champ de glace Juneau dont il est le plus grand glacier et l'un glaciers c\u00F4tiers les plus m\u00E9ridionaux de l'h\u00E9misph\u00E8re nord."@fr . . . . . "Il ghiacciaio Taku si trova nello Stato dell'Alaska, poco a sud-est della citt\u00E0 di Juneau.\u00C8 un ghiacciaio artico in avanzamento, ampio 428 km\u00B2 con una lunghezza di 92 km, che termina nel fiume omonimo. In origine si chiamava Schultze (nel 1883) e Foster (nel 1890), poi per\u00F2 ha prevalso il nome Taku, datogli dai nativi Tlingit."@it . . . . . . "Taku Glacier 1992.jpg"@en . . . . "Taku Glacier (Ling\u00EDt: T'aa\u1E35\u00FA \u1E34w\u00E1an S\u00EDt'i) is a tidewater glacier located in Taku Inlet in the U.S. state of Alaska, just southeast of the city of Juneau. Recognized as the deepest and thickest alpine temperate glacier known in the world, the Taku Glacier is measured at 4,845 feet (1,477 m) thick. It is about 58 kilometres (36 mi) long, and is largely within the Tongass National Forest. Taku Glacier is the namesake of the Alaska Marine Highway System ferry M/V Taku. Taku Glacier was reported to be in retreat as of 2019."@en . "Taku Glacier"@en . . "top"@en . . . . "58.59500122070312"^^ . . . . . . . . . "Il ghiacciaio Taku si trova nello Stato dell'Alaska, poco a sud-est della citt\u00E0 di Juneau.\u00C8 un ghiacciaio artico in avanzamento, ampio 428 km\u00B2 con una lunghezza di 92 km, che termina nel fiume omonimo. In origine si chiamava Schultze (nel 1883) e Foster (nel 1890), poi per\u00F2 ha prevalso il nome Taku, datogli dai nativi Tlingit."@it . "Ghiacciaio Taku"@it . . . . . . . . . . . "Glacier Taku"@fr . "58.595 -134.1797222222222" . "Taku-Gletscher"@de . . . "3300332"^^ . . . . . . . . . . . . "Tidewater glacier"@en . . . "\u5854\u5E93\u51B0\u5DDD\uFF08\u82F1\u8A9E\uFF1ATaku Glacier\uFF09\u662F\u7F8E\u56FD\u963F\u62C9\u65AF\u52A0\u5DDE\u6731\u8BFA\u5E02\u53BF\u7684\uFF0C\u4F4D\u4E8E\uFF0C\u9762\u79EF386\u5E73\u65B9\u82F1\u91CC\uFF081,000\u5E73\u65B9\u516C\u91CC\uFF09\uFF0C\u957F36\u82F1\u91CC\uFF0858\u516C\u91CC\uFF09\u3001\u539A4,845\u82F1\u5C3A\uFF081,477\u7C73\uFF09\uFF0C\u662F\u5168\u4E16\u754C\u6700\u6DF1\u548C\u6700\u539A\u7684\u9AD8\u5C71\u6E29\u5E26\u51B0\u5DDD\uFF0C\u6700\u7EC8\u6CE8\u5165\u3002\u8BE5\u51B0\u5DDD\u7684\u5927\u90E8\u5206\u90FD\u5728\u901A\u52A0\u65AF\u56FD\u5BB6\u68EE\u6797\u5185\u3002"@zh . . . "Der Taku-Gletscher ist ein 58 km langer Gletscher in den Boundary Ranges \u00F6stlich von Juneau in Alaska. Er ist der gr\u00F6\u00DFte Auslassgletscher des Juneau Icefield."@de . . . "O glaciar Taku \u00E9 um glaciar de mar\u00E9 situado a sudeste da cidade de Juneau, no Alasca. O glaciar foi inicialmente (1883) baptizado glaciar Schultze e em 1890 glaciar Foster, mas seria a designa\u00E7\u00E3o dada ao glaciar pelos nativos tlingit, Taku, que acabaria tornando-se a designa\u00E7\u00E3o mais comum. Flui desde o campo de gelo Juneau, sendo o maior dos glaciares de descarga deste campo de gelo e um dos glaciares de mar\u00E9 mais meridionais do hemisf\u00E9rio norte."@pt . . . . . "\u5854\u5E93\u51B0\u5DDD\uFF08\u82F1\u8A9E\uFF1ATaku Glacier\uFF09\u662F\u7F8E\u56FD\u963F\u62C9\u65AF\u52A0\u5DDE\u6731\u8BFA\u5E02\u53BF\u7684\uFF0C\u4F4D\u4E8E\uFF0C\u9762\u79EF386\u5E73\u65B9\u82F1\u91CC\uFF081,000\u5E73\u65B9\u516C\u91CC\uFF09\uFF0C\u957F36\u82F1\u91CC\uFF0858\u516C\u91CC\uFF09\u3001\u539A4,845\u82F1\u5C3A\uFF081,477\u7C73\uFF09\uFF0C\u662F\u5168\u4E16\u754C\u6700\u6DF1\u548C\u6700\u539A\u7684\u9AD8\u5C71\u6E29\u5E26\u51B0\u5DDD\uFF0C\u6700\u7EC8\u6CE8\u5165\u3002\u8BE5\u51B0\u5DDD\u7684\u5927\u90E8\u5206\u90FD\u5728\u901A\u52A0\u65AF\u56FD\u5BB6\u68EE\u6797\u5185\u3002"@zh . . . . . . . . . . "-134.1797180175781"^^ . . . "386"^^ . . "Taku Glacier"@en . . . "\u5854\u5E93\u51B0\u5DDD"@zh . . . . . . . "Glaciar Taku"@pt . "Taku Glacier"@en . "Der Taku-Gletscher ist ein 58 km langer Gletscher in den Boundary Ranges \u00F6stlich von Juneau in Alaska. Er ist der gr\u00F6\u00DFte Auslassgletscher des Juneau Icefield."@de . . "Taku Glacier in 1992"@en . "Le glacier Taku est un glacier c\u00F4tier de l'Alaska du Sud-Est, juste au sud-est de la ville de Juneau. Le glacier fut d'abord nomm\u00E9 glacier Schultze en 1883 puis glacier Foster en 1890, mais Taku, le nom que les am\u00E9rindiens Tlingit locaux avaient pour le glacier, s'imposa. Il se trouve dans la cha\u00EEne C\u00F4ti\u00E8re (Coast Mountains) et prend naissance dans le champ de glace Juneau dont il est le plus grand glacier et l'un glaciers c\u00F4tiers les plus m\u00E9ridionaux de l'h\u00E9misph\u00E8re nord. Le glacier, qui converge vers la Taku River dans la baie Taku (Taku Inlet), a plusieurs fois progress\u00E9, dans son histoire, jusqu'\u00E0 ce qu'il bloque la rivi\u00E8re, cr\u00E9ant un lac, suivi par une dramatique rupture du barrage de glace. La plus r\u00E9cente de ces avanc\u00E9es du glacier date de 1750. Le glacier a avanc\u00E9 de 7,5 kilom\u00E8tres depuis 1890. C'est le seul glacier qui avance des 20 plus importants glaciers provenant du Juneau Icefield. Si cette avance continue, il bloquera de nouveau la rivi\u00E8re. Depuis 1946, le glacier est observ\u00E9 annuellement par le Juneau Icefield Research Program, qui a not\u00E9 une avance du glacier depuis 1988 de 17 m\u00E8tres par an. Cette avance est provoqu\u00E9e par un \u00E9quilibre positif de la masse du glacier (plus de glace qui se forme que de glace qui fond). Jusqu'\u00E0 pr\u00E9sent, le glacier, du fait de cet \u00E9quilibre de masse positif, semblait insensible au r\u00E9chauffement climatique qui touche tous les autres glaciers environnants. La r\u00E9cente inversion de cet \u00E9quilibre entre 1989 et 2005 n'est pas encore suffisante pour arr\u00EAter cette avance mais est sans doute le premier signe que le glacier ne progressera plus dans l'avenir."@fr . . "1087663837"^^ . "Taku Glacier (Ling\u00EDt: T'aa\u1E35\u00FA \u1E34w\u00E1an S\u00EDt'i) is a tidewater glacier located in Taku Inlet in the U.S. state of Alaska, just southeast of the city of Juneau. Recognized as the deepest and thickest alpine temperate glacier known in the world, the Taku Glacier is measured at 4,845 feet (1,477 m) thick. It is about 58 kilometres (36 mi) long, and is largely within the Tongass National Forest. The glacier was originally named Schultze Glacier in 1883 and the Foster Glacier in 1890, but Taku, the name the local Tlingit natives had for the glacier, eventually stuck. It is nestled in the Coast Mountains and originates in the Juneau Icefield. It is the largest glacier in the icefield and one of the southernmost tidewater glaciers of the northern hemisphere. The glacier, which converges with the Taku River at Taku Inlet, has a history of advancing until it blocks the river, creating a lake, followed by a dramatic break of the ice dam. The most recent of these advances occurred in 1750. The glacier has advanced 7.75 kilometres (4.82 mi) since 1890, and as of June 29, 2012 is 1.26 kilometres (0.78 mi) from Taku Point. It is the only advancing glacier of the 20 major glaciers of the Juneau Icefield. If the advance continues it will again block the river, but this appears unlikely at present. Since 1946, the glacier has been monitored by the Juneau Icefield Research Program, which has documented its rate of advance since 1988 at 17 metres (56 ft) a year. The advance is due to a positive mass balance; that is, more snow accumulates than snow and ice melt. Until 1948 the glacier had a calving front; since then the terminus has been grounded. Due to the positive mass balance and the fact that it was no longer losing mass to icebergs, Taku Glacier has become insensitive to the warming that has impacted all other glaciers of the icefield. This has driven its advance. The recent negative mass balance 1989-2005 is not large enough yet to stop the advance, but it is the first sign that the glacier's advance may not take it to Taku Point. Taku Glacier is the namesake of the Alaska Marine Highway System ferry M/V Taku. Taku Glacier was reported to be in retreat as of 2019."@en . . . . "T'aa\u1E35\u00FA \u1E34w\u00E1an S\u00EDt'i"@en . . . "Retreating"@en . "58.0"^^ . . "POINT(-134.17971801758 58.595001220703)"^^ .