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- Q191110 subject Q7037488.
- Q191110 subject Q8425760.
- Q191110 abstract "A craton (/ˈkreɪtɒn/, /ˈkrætɒn/, or /ˈkreɪtən/; from Greek: κράτος kratos "strength") is an old and stable part of the continental lithosphere. Having often survived cycles of merging and rifting of continents, cratons are generally found in the interiors of tectonic plates. They are characteristically composed of ancient crystalline basement rock, which may be covered by younger sedimentary rock. They have a thick crust and deep lithospheric roots that extend as much as several hundred kilometres into the Earth's mantle.The term craton is used to distinguish the stable portion of the continental crust from regions that are more geologically active and unstable. Cratons can be described as shields, in which the basement rock crops out at the surface, and platforms, in which the basement is overlaid by sediments and sedimentary rock.The word craton was first proposed by the Austrian geologist Leopold Kober in 1921 as Kratogen, referring to stable continental platforms, and orogen as a term for mountain or orogenic belts. Later authors shortened the former term to kraton and then to craton.Examples of cratons are the Slave Craton in Canada, the Wyoming Craton in the United States, the Amazonia Craton in South America, the Kaapvaal Craton in South Africa, and the Gawler Craton in South Australia.".
- Q191110 wikiPageExternalLink deliverPDF.jsp?docId=33717&courseCode=GEOG11023.
- Q191110 wikiPageExternalLink 4_1_3_1.html.
- Q191110 wikiPageExternalLink Continental_Hearts.
- Q191110 wikiPageExternalLink 140.html.
- Q191110 wikiPageExternalLink sdarticle.pdf.
- Q191110 wikiPageWikiLink Q101949.
- Q191110 wikiPageWikiLink Q104168.
- Q191110 wikiPageWikiLink Q105131.
- Q191110 wikiPageWikiLink Q108689.
- Q191110 wikiPageWikiLink Q1143398.
- Q191110 wikiPageWikiLink Q1409210.
- Q191110 wikiPageWikiLink Q16.
- Q191110 wikiPageWikiLink Q166257.
- Q191110 wikiPageWikiLink Q176318.
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- Q191110 wikiPageWikiLink Q7037488.
- Q191110 wikiPageWikiLink Q728944.
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- Q191110 wikiPageWikiLink Q81659.
- Q191110 wikiPageWikiLink Q82480.
- Q191110 wikiPageWikiLink Q83296.
- Q191110 wikiPageWikiLink Q8425760.
- Q191110 wikiPageWikiLink Q847257.
- Q191110 wikiPageWikiLink Q8502.
- Q191110 wikiPageWikiLink Q852013.
- Q191110 wikiPageWikiLink Q858571.
- Q191110 wikiPageWikiLink Q878045.
- Q191110 wikiPageWikiLink Q89418.
- Q191110 type Thing.
- Q191110 comment "A craton (/ˈkreɪtɒn/, /ˈkrætɒn/, or /ˈkreɪtən/; from Greek: κράτος kratos "strength") is an old and stable part of the continental lithosphere. Having often survived cycles of merging and rifting of continents, cratons are generally found in the interiors of tectonic plates. They are characteristically composed of ancient crystalline basement rock, which may be covered by younger sedimentary rock.".
- Q191110 label "Craton".