Late Quaternary loess landscape evolution on an active tectonic margin, Charwell Basin, South Island, New Zealand Reconstruction of landscape change in Quaternary environments

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Published in:Geomorphology (Amsterdam, Netherlands) Vol. 122; no. 3-4; pp. 294 - 308
Main Authors: HUGHES, Matthew W, ALMOND, Peter C, ROERING, Joshua J, TONKIN, Philip J
Format: Journal Article
Language:English
Published: Amsterdam Elsevier 2010
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Author HUGHES, Matthew W
ROERING, Joshua J
ALMOND, Peter C
TONKIN, Philip J
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  organization: Department of Soil and Physical Sciences, PO Box 84, Lincoln University, Lincoln 7647, Canterbury, New Zealand
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  givenname: Peter C
  surname: ALMOND
  fullname: ALMOND, Peter C
  organization: Department of Soil and Physical Sciences, PO Box 84, Lincoln University, Lincoln 7647, Canterbury, New Zealand
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  givenname: Joshua J
  surname: ROERING
  fullname: ROERING, Joshua J
  organization: Department of Geological Sciences, University of Oregon, Eugene, OR 97403-1272, United States
– sequence: 4
  givenname: Philip J
  surname: TONKIN
  fullname: TONKIN, Philip J
  organization: Department of Geological Sciences, University of Canterbury, Private Bag 4800, Christchurch, New Zealand
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Issue 3-4
Keywords thickness
Australasia
loess
Alluvial terraces
drainage patterns
upper Quaternary
faults
fluvial sedimentation
tectonics
terraces
Cenozoic
soils
landscapes
tectonic controls
models
morphology
Quaternary
accumulation
digital elevation models
transport
erosion rates
landforms
floodplains
Active tectonics
Landscape evolution
erosion
Phanerozoic
valleys
Language English
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PublicationPlace Amsterdam
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PublicationTitle Geomorphology (Amsterdam, Netherlands)
PublicationYear 2010
Publisher Elsevier
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StartPage 294
SubjectTerms Earth sciences
Earth, ocean, space
Exact sciences and technology
Geomorphology, landform evolution
Marine and continental quaternary
Surficial geology
Tectonics. Structural geology. Plate tectonics
Subtitle Reconstruction of landscape change in Quaternary environments
Title Late Quaternary loess landscape evolution on an active tectonic margin, Charwell Basin, South Island, New Zealand
Volume 122
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