Cascade Bluff (84°57′S 178°10′W / 84.950°S 178.167°W) is a low, mainly ice-covered bluff that forms the southwest wall of Mincey Glacier in the Queen Maud Mountains in Antarctica. The feature was so named by the Texas Tech Shackleton Glacier Expedition, 1962–63, because water cascades over the bluff during warm periods.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Cascade Bluff (de)
- Cascade Bluff (en)
- Cascade Bluff (it)
- 喀斯喀特海崖 (zh)
|
| rdfs:comment
| - Das Cascade Bluff ist ein niedriges und hauptsächlich vereistes Felsenkliff in der antarktischen Ross Dependency. Im Königin-Maud-Gebirge bildet es die Südwestwand des Mincey-Gletschers. Teilnehmer der von der Texas Tech University unternommenen Expedition zum Shackleton-Gletscher (1962–1963) benannten es so, da bei warmen Wetter Schmelzwasser in Form einer Kaskade über das Kliff hinabstürzt. (de)
- Cascade Bluff (84°57′S 178°10′W / 84.950°S 178.167°W) is a low, mainly ice-covered bluff that forms the southwest wall of Mincey Glacier in the Queen Maud Mountains in Antarctica. The feature was so named by the Texas Tech Shackleton Glacier Expedition, 1962–63, because water cascades over the bluff during warm periods. (en)
- La Cascade Bluff (in lingua inglese: falesia delle cascate) è una bassa falesia antartica, per lo più ricoperta di ghiaccio, che forma la parete del fianco sudoccidentale del Ghiacciaio Mincey, nei Monti della Regina Maud, in Antartide. La denominazione è stata assegnata dalla Texas Tech Shackleton Glacier Expedition, la spedizione antartica sul Ghiacciaio Shackleton della Texas Tech University del 1962-63, a causa della cascatelle formate dall'acqua di fusione che si originano sulla scogliera durante la stagione calda. (it)
- 喀斯喀特海崖（英語：Cascade Bluff），是南極洲的海崖，位於杜費克海岸，處於明塞冰川西南岸，屬於毛德王后山脈的一部分，現時由南極條約體系管理。 (zh)
|
| geo:lat
| |
| geo:long
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| georss:point
| - -84.95 -178.16666666666666
|
| has abstract
| - Das Cascade Bluff ist ein niedriges und hauptsächlich vereistes Felsenkliff in der antarktischen Ross Dependency. Im Königin-Maud-Gebirge bildet es die Südwestwand des Mincey-Gletschers. Teilnehmer der von der Texas Tech University unternommenen Expedition zum Shackleton-Gletscher (1962–1963) benannten es so, da bei warmen Wetter Schmelzwasser in Form einer Kaskade über das Kliff hinabstürzt. (de)
- Cascade Bluff (84°57′S 178°10′W / 84.950°S 178.167°W) is a low, mainly ice-covered bluff that forms the southwest wall of Mincey Glacier in the Queen Maud Mountains in Antarctica. The feature was so named by the Texas Tech Shackleton Glacier Expedition, 1962–63, because water cascades over the bluff during warm periods. (en)
- La Cascade Bluff (in lingua inglese: falesia delle cascate) è una bassa falesia antartica, per lo più ricoperta di ghiaccio, che forma la parete del fianco sudoccidentale del Ghiacciaio Mincey, nei Monti della Regina Maud, in Antartide. La denominazione è stata assegnata dalla Texas Tech Shackleton Glacier Expedition, la spedizione antartica sul Ghiacciaio Shackleton della Texas Tech University del 1962-63, a causa della cascatelle formate dall'acqua di fusione che si originano sulla scogliera durante la stagione calda. (it)
- 喀斯喀特海崖（英語：Cascade Bluff），是南極洲的海崖，位於杜費克海岸，處於明塞冰川西南岸，屬於毛德王后山脈的一部分，現時由南極條約體系管理。 (zh)
|
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| geo:geometry
| - POINT(-178.16667175293 -84.949996948242)
|
| is Link from a Wikipage to another Wikipage
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)