1972
DOI: 10.1080/00167617208728773
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Soil and landscape studies in Western Australia

Abstract: The main features of climate and geology relevant to a discussion of the soils and landscapes of Western Australia are briefly reviewed. The pattern of drainage is described in terms of six drainage divisions, each with characteristic physiography and soils. In the interior, this involves a reconstruction of an ancient drainage system, based on the maps of the Atlas of Australian Soils. It is shown, on a continental scale, that the major divides are characterised not only by deep, chemically weathered, often l… Show more

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Cited by 29 publications
(10 citation statements)
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“…The region consists of many ancient, steep-sided mountain ranges that are heavily dissected by riverfloodplain systems that reliably discharge surface water into the coastal marine zone. Regional geology is complex and contains some of the oldest rock deposits (e.g., Phanerozoic, Proterozoic, and Archaean sedimentary, granite, and volcanic rocks and Devonian limestone) in the world, some as old as 3.7 yr BP (Mulcahy and Bettenay 1972). Soils are generally heavily weathered vertisols with low organic matter contents.…”
Section: Methodsmentioning
confidence: 99%
“…The region consists of many ancient, steep-sided mountain ranges that are heavily dissected by riverfloodplain systems that reliably discharge surface water into the coastal marine zone. Regional geology is complex and contains some of the oldest rock deposits (e.g., Phanerozoic, Proterozoic, and Archaean sedimentary, granite, and volcanic rocks and Devonian limestone) in the world, some as old as 3.7 yr BP (Mulcahy and Bettenay 1972). Soils are generally heavily weathered vertisols with low organic matter contents.…”
Section: Methodsmentioning
confidence: 99%
“…Approximately 67% of the native forest has been cleared for farmland (Loh et al 1989). The landscape and soils of these sites are typical of the Beraking valley form, with slopes dominated by gravelly, sandy soils and some ferruginous duricrust on the hilltops (Mulcahy & Bettenay 1972). The sites are at the eastern extent of the northern jarrah forest where jarrah ( E. marginata ) and to a lesser extent marri ( E. calophylla ) and wandoo ( Eucalyptus wandoo ) form woodland or open forest (Dell & Havel 1989).…”
Section: Methodsmentioning
confidence: 99%
“…The landscape and soils of these sites are typical of the Beraking valley form with slopes dominated by gravelly sandy soils with some ferruginous duricrust on the hilltops (Mulcahy & Bettenay 1972) . The sites are at the eastern extent of the northern jarrah forest where Eucalyptus marginata (jarrah) and to a lesser extent E. calophylla (marri) and E. wandoo (wandoo) form a woodland or open forest (Dell & Havel 1989).…”
Section: Methodsmentioning
confidence: 99%