Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/63746
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dc.contributor.authorBrock, E.en
dc.contributor.authorTwidale, C.en
dc.date.issued2011en
dc.identifier.citationGeographical Research, 2011; 49(1):1-12en
dc.identifier.issn1745-5871en
dc.identifier.issn1745-5863en
dc.identifier.urihttp://hdl.handle.net/2440/63746-
dc.description.abstractFor a brief period about a century ago, reputable scientists gave credence to the idea that wind was capable of regional planation. Among them was J.T. Jutson, whose publications exerted considerable influence both in Australia and overseas. He differentiated between deflation and corrasion (sand-blasting) and in 1914 attributed major as well as minor landscape features to their activity. He ascribed the westward migration of salinas and the shaping of associated rock platforms to the wind as well as to the extension of valleys that were incised into the lateritised Old Plateau and that coalesced to form the New Plateau of Western Australia. But local and overseas colleagues drew his attention to the primacy of rivers in shaping even desert landscapes, and by 1934 Jutson had realised that running water was almost solely responsible for the New Plateau.en
dc.description.statementofresponsibilityE. J. Brock and C. R. Twidaleen
dc.language.isoenen
dc.publisherWiley-Blackwell Publishing Asiaen
dc.rights© 2010 The Authorsen
dc.subjectJutson; work of wind; deflation; corrasion; Old and New plateaux; migration of lakes; work of riversen
dc.titleJ.T. Jutson and the work of the wind in shaping the landscapeen
dc.typeJournal articleen
dc.identifier.rmid0020104916en
dc.identifier.doi10.1111/j.1745-5871.2010.00662.xen
dc.identifier.pubid31395-
pubs.library.collectionGeology & Geophysics publicationsen
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
Appears in Collections:Geology & Geophysics publications

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