Matches in DBpedia 2016-04 for { ?s ?p "Giant current ripples are active channel topographic forms up to 20 m high, which develop within near-talweg areas of the main outflow valleys created by glacial lake outburst floods. Giant current ripple marks are morphologic and genetic macroanalogues of small current ripples formed in sandy stream sediments.The giant current ripple marks are important depositional forms in diluvial plain and mountain scablands."@en }
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- Giant_current_ripples abstract "Giant current ripples are active channel topographic forms up to 20 m high, which develop within near-talweg areas of the main outflow valleys created by glacial lake outburst floods. Giant current ripple marks are morphologic and genetic macroanalogues of small current ripples formed in sandy stream sediments.The giant current ripple marks are important depositional forms in diluvial plain and mountain scablands.".
- Q4137986 abstract "Giant current ripples are active channel topographic forms up to 20 m high, which develop within near-talweg areas of the main outflow valleys created by glacial lake outburst floods. Giant current ripple marks are morphologic and genetic macroanalogues of small current ripples formed in sandy stream sediments.The giant current ripple marks are important depositional forms in diluvial plain and mountain scablands.".
- Giant_current_ripples comment "Giant current ripples are active channel topographic forms up to 20 m high, which develop within near-talweg areas of the main outflow valleys created by glacial lake outburst floods. Giant current ripple marks are morphologic and genetic macroanalogues of small current ripples formed in sandy stream sediments.The giant current ripple marks are important depositional forms in diluvial plain and mountain scablands.".
- Q4137986 comment "Giant current ripples are active channel topographic forms up to 20 m high, which develop within near-talweg areas of the main outflow valleys created by glacial lake outburst floods. Giant current ripple marks are morphologic and genetic macroanalogues of small current ripples formed in sandy stream sediments.The giant current ripple marks are important depositional forms in diluvial plain and mountain scablands.".