Otway Massif (85°27′S 172°0′E / 85.450°S 172.000°E) is a prominent, mainly ice-free massif, about 10 nautical miles (18 km) long and 7 nautical miles (13 km) wide, standing at the northwest end of the Grosvenor Mountains at the confluence of Mill Glacier and Mill Stream Glacier. Surveyed and named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for , who had wintered over at Scott Base and was a member of this party and the Northern Party during the summer of 1960–61.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Otway-Massiv (de)
- Otway Massif (it)
- Otway Massif (en)
- Otway Massif (sv)
- 奧特韋山 (zh)
|
| rdfs:comment
| - Das Otway-Massiv ist ein markantes, hauptsächlich eisfreies und 3200 m hohes Bergmassiv mit einer Ausdehnung von rund 112 km² in der antarktischen Ross Dependency. Es ragt am Zusammenfluss von Mill-Gletscher und Mill-Stream-Gletscher am nordwestlichen Ende der Grosvenor Mountains auf. Erkundet und benannt wurde es von der Südgruppe einer von 1961 bis 1962 durchgeführten Kampagne im Rahmen der New Zealand Geological Survey Antarctic Expedition. Benannt ist es nach Peter Miles Otway (* 1936), einem Teilnehmer der Expedition. (de)
- Otway Massif (85°27′S 172°0′E / 85.450°S 172.000°E) is a prominent, mainly ice-free massif, about 10 nautical miles (18 km) long and 7 nautical miles (13 km) wide, standing at the northwest end of the Grosvenor Mountains at the confluence of Mill Glacier and Mill Stream Glacier. Surveyed and named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for , who had wintered over at Scott Base and was a member of this party and the Northern Party during the summer of 1960–61. (en)
- Otway Massif är en bergskedja i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. (sv)
- 奧特韋山（英語：Otway Massif）是南極洲的山峰，位於杜費克海岸，屬於格羅夫納山脈的一部分，長18公里、寬13公里，處於米爾冰川和米爾斯特里姆冰川的匯流處，由新西蘭探險隊命名。 (zh)
- L'Otway Massif è un imponente massiccio, prevalentemente privo di ghiaccio, lungo circa 18 km e largo circa 13 km, situato alla confluenza del Ghiacciaio Mill e del Ghiacciaio Mill Stream, all'estremità nordoccidentale delle Grosvenor Mountains, catena montuosa che fa parte dei Monti della Regina Maud, in Antartide. (it)
|
| geo:lat
| |
| geo:long
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| georss:point
| |
| has abstract
| - Das Otway-Massiv ist ein markantes, hauptsächlich eisfreies und 3200 m hohes Bergmassiv mit einer Ausdehnung von rund 112 km² in der antarktischen Ross Dependency. Es ragt am Zusammenfluss von Mill-Gletscher und Mill-Stream-Gletscher am nordwestlichen Ende der Grosvenor Mountains auf. Erkundet und benannt wurde es von der Südgruppe einer von 1961 bis 1962 durchgeführten Kampagne im Rahmen der New Zealand Geological Survey Antarctic Expedition. Benannt ist es nach Peter Miles Otway (* 1936), einem Teilnehmer der Expedition. (de)
- Otway Massif (85°27′S 172°0′E / 85.450°S 172.000°E) is a prominent, mainly ice-free massif, about 10 nautical miles (18 km) long and 7 nautical miles (13 km) wide, standing at the northwest end of the Grosvenor Mountains at the confluence of Mill Glacier and Mill Stream Glacier. Surveyed and named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for , who had wintered over at Scott Base and was a member of this party and the Northern Party during the summer of 1960–61. (en)
- L'Otway Massif è un imponente massiccio, prevalentemente privo di ghiaccio, lungo circa 18 km e largo circa 13 km, situato alla confluenza del Ghiacciaio Mill e del Ghiacciaio Mill Stream, all'estremità nordoccidentale delle Grosvenor Mountains, catena montuosa che fa parte dei Monti della Regina Maud, in Antartide. Fu scoperto dal gruppo che seguiva il percorso Sud nel corso della New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62).La denominazione è stata assegnata in onore di Peter Miles Otway (* 1936-), che aveva trascorso l'inverno nella Base Scott con il suo gruppo ed entrò poi a far parte del gruppo che seguiva il percorso Nord durante l'estate 1960-61. (it)
- Otway Massif är en bergskedja i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. (sv)
- 奧特韋山（英語：Otway Massif）是南極洲的山峰，位於杜費克海岸，屬於格羅夫納山脈的一部分，長18公里、寬13公里，處於米爾冰川和米爾斯特里姆冰川的匯流處，由新西蘭探險隊命名。 (zh)
|
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| geo:geometry
| - POINT(172 -85.449996948242)
|
| is Link from a Wikipage to another Wikipage
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)