Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q256438> ?p ?o }
Showing triples 1 to 81 of
81
with 100 triples per page.
- Q256438 subject Q19826743.
- Q256438 subject Q6802033.
- Q256438 abstract "An ignimbrite is the deposit of a pyroclastic density current, or pyroclastic flow, which is a hot suspension of particles and gases flowing rapidly from a volcano driven by having a greater density than the surrounding atmosphere. New Zealand geologist Patrick Marshall derived the term 'ignimbrite' from ‘fiery rock dust cloud’ (from the Latin igni- (fire) and imbri- (rain)), formed as the result of immense explosions of pyroclastic ash, lapilli and blocks flowing down the sides of volcanoes.Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated or lithified (solidified) rock called lapilli-tuff. Proximal to the volcanic source, ignimbrites commonly contain thick accumulations of lithic blocks, and distally, many show meter thick accumulations of rounded cobbles of pumice.Ignimbrites may be white, grey, pink, beige, brown or black depending on their composition and density. Many pale ignimbrites are dacitic or rhyolitic. Darker coloured ignimbrites may be densely welded volcanic glass or, less commonly, mafic in composition.".
- Q256438 thumbnail BishopTuff.jpg?width=300.
- Q256438 wikiPageExternalLink ignimbrite_intro.html.
- Q256438 wikiPageExternalLink default.asp?Find_Quick.asp?PersonEssay=3M44.
- Q256438 wikiPageWikiLink Q1036221.
- Q256438 wikiPageWikiLink Q1049667.
- Q256438 wikiPageWikiLink Q1057300.
- Q256438 wikiPageWikiLink Q105880.
- Q256438 wikiPageWikiLink Q107099.
- Q256438 wikiPageWikiLink Q107749.
- Q256438 wikiPageWikiLink Q1124584.
- Q256438 wikiPageWikiLink Q1134464.
- Q256438 wikiPageWikiLink Q1191052.
- Q256438 wikiPageWikiLink Q1227.
- Q256438 wikiPageWikiLink Q1257550.
- Q256438 wikiPageWikiLink Q128709.
- Q256438 wikiPageWikiLink Q1322038.
- Q256438 wikiPageWikiLink Q133738.
- Q256438 wikiPageWikiLink Q1522.
- Q256438 wikiPageWikiLink Q159954.
- Q256438 wikiPageWikiLink Q1638164.
- Q256438 wikiPageWikiLink Q170258.
- Q256438 wikiPageWikiLink Q178925.
- Q256438 wikiPageWikiLink Q180044.
- Q256438 wikiPageWikiLink Q183360.
- Q256438 wikiPageWikiLink Q189452.
- Q256438 wikiPageWikiLink Q190727.
- Q256438 wikiPageWikiLink Q191250.
- Q256438 wikiPageWikiLink Q192880.
- Q256438 wikiPageWikiLink Q19826743.
- Q256438 wikiPageWikiLink Q206492.
- Q256438 wikiPageWikiLink Q209245.
- Q256438 wikiPageWikiLink Q210510.
- Q256438 wikiPageWikiLink Q2142173.
- Q256438 wikiPageWikiLink Q2158896.
- Q256438 wikiPageWikiLink Q221616.
- Q256438 wikiPageWikiLink Q222814.
- Q256438 wikiPageWikiLink Q223197.
- Q256438 wikiPageWikiLink Q256438.
- Q256438 wikiPageWikiLink Q29539.
- Q256438 wikiPageWikiLink Q30.
- Q256438 wikiPageWikiLink Q3224.
- Q256438 wikiPageWikiLink Q325173.
- Q256438 wikiPageWikiLink Q36133.
- Q256438 wikiPageWikiLink Q383481.
- Q256438 wikiPageWikiLink Q397.
- Q256438 wikiPageWikiLink Q40157.
- Q256438 wikiPageWikiLink Q407339.
- Q256438 wikiPageWikiLink Q408.
- Q256438 wikiPageWikiLink Q410893.
- Q256438 wikiPageWikiLink Q419201.
- Q256438 wikiPageWikiLink Q422075.
- Q256438 wikiPageWikiLink Q42278.
- Q256438 wikiPageWikiLink Q43010.
- Q256438 wikiPageWikiLink Q43338.
- Q256438 wikiPageWikiLink Q4493802.
- Q256438 wikiPageWikiLink Q457931.
- Q256438 wikiPageWikiLink Q466481.
- Q256438 wikiPageWikiLink Q481758.
- Q256438 wikiPageWikiLink Q484924.
- Q256438 wikiPageWikiLink Q488640.
- Q256438 wikiPageWikiLink Q495423.
- Q256438 wikiPageWikiLink Q512121.
- Q256438 wikiPageWikiLink Q580585.
- Q256438 wikiPageWikiLink Q650836.
- Q256438 wikiPageWikiLink Q664.
- Q256438 wikiPageWikiLink Q6802033.
- Q256438 wikiPageWikiLink Q692922.
- Q256438 wikiPageWikiLink Q7147110.
- Q256438 wikiPageWikiLink Q764372.
- Q256438 wikiPageWikiLink Q8072.
- Q256438 wikiPageWikiLink Q810178.
- Q256438 wikiPageWikiLink Q816.
- Q256438 wikiPageWikiLink Q829.
- Q256438 wikiPageWikiLink Q83471.
- Q256438 wikiPageWikiLink Q843607.
- Q256438 comment "An ignimbrite is the deposit of a pyroclastic density current, or pyroclastic flow, which is a hot suspension of particles and gases flowing rapidly from a volcano driven by having a greater density than the surrounding atmosphere.".
- Q256438 label "Ignimbrite".
- Q256438 depiction BishopTuff.jpg.