Matches in DBpedia 2016-04 for { <http://dbpedia.org/resource/Subglacial_stream> ?p ?o }
Showing triples 1 to 30 of
30
with 100 triples per page.
- Subglacial_stream abstract "Subglacial streams are streams which flow in a channel at the bottom of an ice-sheet or a glacier, and are usually close to the glacier terminus or snout. These are fed by streams on top of the glacier which descend through ducts in the ice. The pressures are very high in these streams due to the huge mass of ice above them, consequently, they have very high erosive power meaning they will increase the volume of water flowing through, maintaining the high pressure. Some subglacial streams have the strange property of 'flowing' uphill due to the colossal pressures that are present.".
- Subglacial_stream wikiPageID "31213939".
- Subglacial_stream wikiPageLength "962".
- Subglacial_stream wikiPageOutDegree "6".
- Subglacial_stream wikiPageRevisionID "490592773".
- Subglacial_stream wikiPageWikiLink Category:Glacial_landforms.
- Subglacial_stream wikiPageWikiLink Category:Glaciers.
- Subglacial_stream wikiPageWikiLink Category:Montane_ecology.
- Subglacial_stream wikiPageWikiLink Glacier.
- Subglacial_stream wikiPageWikiLink Glacier_terminus.
- Subglacial_stream wikiPageWikiLink Ice_sheet.
- Subglacial_stream wikiPageWikiLinkText "Subglacial stream".
- Subglacial_stream wikiPageWikiLinkText "sub-glacial flow".
- Subglacial_stream wikiPageWikiLinkText "subglacial stream".
- Subglacial_stream wikiPageUsesTemplate Template:Glaciers.
- Subglacial_stream wikiPageUsesTemplate Template:Reflist.
- Subglacial_stream subject Category:Glacial_landforms.
- Subglacial_stream subject Category:Glaciers.
- Subglacial_stream subject Category:Montane_ecology.
- Subglacial_stream hypernym Streams.
- Subglacial_stream type River.
- Subglacial_stream type Landform.
- Subglacial_stream type Subfield.
- Subglacial_stream comment "Subglacial streams are streams which flow in a channel at the bottom of an ice-sheet or a glacier, and are usually close to the glacier terminus or snout. These are fed by streams on top of the glacier which descend through ducts in the ice. The pressures are very high in these streams due to the huge mass of ice above them, consequently, they have very high erosive power meaning they will increase the volume of water flowing through, maintaining the high pressure.".
- Subglacial_stream label "Subglacial stream".
- Subglacial_stream sameAs Q7631148.
- Subglacial_stream sameAs m.0gj8l_v.
- Subglacial_stream sameAs Q7631148.
- Subglacial_stream wasDerivedFrom Subglacial_stream?oldid=490592773.
- Subglacial_stream isPrimaryTopicOf Subglacial_stream.