Smith Glacier is a low-gradient Antarctic glacier, over 160 km (100 mi) long, draining from Toney Mountain in an ENE direction to Amundsen Sea. A northern distributary, Kohler Glacier, drains to Dotson Ice Shelf but the main flow passes to the sea between Bear Peninsula and Mount Murphy, terminating at Crosson Ice Shelf. The Smith Glacier is located in the western region of Antarctica. Latitude: 75° 2' 59'' S. Longitude 111° 12' 0'' W. In 2011, Hamish Pritchard, a scientist with the British Antarctic Survey in Cambridge, UK, said that Smith Glacier was thinning at a rate of 27 feet per year.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Smith-Gletscher (de)
- Ghiacciaio Smith (it)
- Smith Glacier (en)
- Smith Glacier (glaciär i Antarktis) (sv)
- 史密斯冰川 (zh)
|
| rdfs:comment
| - Il ghiacciaio Smith (in inglese Smith Glacier) è un ghiacciaio lungo oltre 160 km situato sulla costa di Walgreen, nella parte orientale della Terra di Marie Byrd, in Antartide. (it)
- Smith Glacier är en glaciär i Antarktis. Den ligger i Västantarktis. Inget land gör anspråk på området. Smith Glacier ligger 75 meter över havet. Terrängen runt Smith Glacier är platt. Den högsta punkten i närheten är 366 meter över havet, 20,0 kilometer söder om Smith Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 史密斯冰川（英語：Smith Glacier）是南極洲的冰川，全長超過160公里，發源自托尼山，朝著東南方向流動，注入阿蒙森海，其支流科勒冰川注入多特森冰架。 (zh)
- Der Smith-Gletscher ist ein 160 km langer Gletscher mit geringem Fließgefälle im westantarktischen Marie-Byrd-Land. Er fließt vom Toney Mountain in ostnordöstlicher Richtung zum Crosson-Schelfeis an der Walgreen-Küste, das er zwischen der Bear-Halbinsel und Mount Murphy erreicht. Der zum Dotson-Schelfeis fließende Kohler-Gletscher ist ein Abzweig des Smith-Gletschers. (de)
- Smith Glacier is a low-gradient Antarctic glacier, over 160 km (100 mi) long, draining from Toney Mountain in an ENE direction to Amundsen Sea. A northern distributary, Kohler Glacier, drains to Dotson Ice Shelf but the main flow passes to the sea between Bear Peninsula and Mount Murphy, terminating at Crosson Ice Shelf. The Smith Glacier is located in the western region of Antarctica. Latitude: 75° 2' 59'' S. Longitude 111° 12' 0'' W. In 2011, Hamish Pritchard, a scientist with the British Antarctic Survey in Cambridge, UK, said that Smith Glacier was thinning at a rate of 27 feet per year. (en)
|
| geo:lat
| |
| geo:long
| |
| location
| |
| dct:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| georss:point
| - -75.08333333333333 -112.0
|
| has abstract
| - Der Smith-Gletscher ist ein 160 km langer Gletscher mit geringem Fließgefälle im westantarktischen Marie-Byrd-Land. Er fließt vom Toney Mountain in ostnordöstlicher Richtung zum Crosson-Schelfeis an der Walgreen-Küste, das er zwischen der Bear-Halbinsel und Mount Murphy erreicht. Der zum Dotson-Schelfeis fließende Kohler-Gletscher ist ein Abzweig des Smith-Gletschers. Der United States Geological Survey kartierte ihn anhand eigener Vermessungen und Luftaufnahmen der United States Navy aus den Jahren von 1959 bis 1965. Das Advisory Committee on Antarctic Names benannte ihn 1967 nach Philip Meek Smith (* 1932), stellvertretender Direktor des Polarprogramms der National Science Foundation, der zwischen 1956 und 1971 an zahlreichen Forschungsreisen in die Antarktis beteiligt war. (de)
- Smith Glacier is a low-gradient Antarctic glacier, over 160 km (100 mi) long, draining from Toney Mountain in an ENE direction to Amundsen Sea. A northern distributary, Kohler Glacier, drains to Dotson Ice Shelf but the main flow passes to the sea between Bear Peninsula and Mount Murphy, terminating at Crosson Ice Shelf. The Smith Glacier is located in the western region of Antarctica. Latitude: 75° 2' 59'' S. Longitude 111° 12' 0'' W. Mapped by USGS from ground surveys and USN air photos, 1959–65. Named by US-ACAN after Philip M. Smith (Smith Bluffs), Deputy Director, Office of Polar Programs, National Science Foundation, who in the period 1956–71 participated in many expeditions to Antarctica in field and supervisory capacities. In 2001, Dr. Andrew Shepherd, a research fellow at the Center for Polar Observation and Modeling at University College London, said that Smith Glacier was losing mass quickly and contributing to the slow rise of the oceans. In 2011, Hamish Pritchard, a scientist with the British Antarctic Survey in Cambridge, UK, said that Smith Glacier was thinning at a rate of 27 feet per year. In 2016, a study published in the journal Nature Communication, which relied on airborne radar measurements, found that melting of the ice shelves’ grounding zones between the years 2000 and 2009 removed between 984 to about 1,607 feet of solid ice beneath the Smith Glacier. The Smith Glacier lost more ice than any other glacier studied for the report. The researchers found that the Smith Glacier retreated by about 21 miles during the period from 1996 to 2011. The scientists concluded that the size of the retreat was partly a result of both the unique topography underneath the ice that allowed more ocean water to sneak in between the ice and the land below. (en)
- Il ghiacciaio Smith (in inglese Smith Glacier) è un ghiacciaio lungo oltre 160 km situato sulla costa di Walgreen, nella parte orientale della Terra di Marie Byrd, in Antartide. (it)
- Smith Glacier är en glaciär i Antarktis. Den ligger i Västantarktis. Inget land gör anspråk på området. Smith Glacier ligger 75 meter över havet. Terrängen runt Smith Glacier är platt. Den högsta punkten i närheten är 366 meter över havet, 20,0 kilometer söder om Smith Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 史密斯冰川（英語：Smith Glacier）是南極洲的冰川，全長超過160公里，發源自托尼山，朝著東南方向流動，注入阿蒙森海，其支流科勒冰川注入多特森冰架。 (zh)
|
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| located in area
| |
| foaf:isPrimaryTopicOf
| |
| geo:geometry
| - POINT(-112 -75.083335876465)
|
| is Link from a Wikipage to another Wikipage
of | |
| is Wikipage redirect
of | |
| is Wikipage disambiguates
of | |
| is foaf:primaryTopic
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)