Show simple item record  

dc.contributor.authorClaessens, L.
dc.contributor.authorLowe, David J.
dc.contributor.authorHayward, B.W.
dc.contributor.authorSchaap, B.F.
dc.contributor.authorSchoorl, J.M.
dc.contributor.authorVeldkamp, A.
dc.date.accessioned2008-08-07T03:28:52Z
dc.date.available2008-08-07T03:28:52Z
dc.date.issued2006-03
dc.identifier.citationClaessens, L., Lowe, D.J., Hayward, B.W., Schoorl, J.M. & Veldkamp, A. (2006). Reconstructing high-magnitude/low-frequency landslide events based on soil redistribution modelling and a Late-Holocene sediment record from New Zealand. Geomorphology 74, 29-49.en_US
dc.identifier.issn0169-555X
dc.identifier.urihttps://hdl.handle.net/10289/929
dc.description.abstractA sediment record is used, in combination with shallow landslide soil redistribution and sediment-yield modelling, to reconstruct the incidence of high-magnitude/low-frequency landslide events in the upper part of a catchment and the history of a wetland in the lower part. Eleven sediment cores were obtained from a dune-impounded wetland at Te Henga, west Auckland, northern New Zealand. Sediment stratigraphy and chronology were interpreted by radiocarbon dating, foraminiferal analysis, and provisional tephrochronology. Gradual impoundment of the wetland began c. 6000 cal yr BP, coinciding with the start of a gentle sea-level fall, but complete damming and initial sedimentation did not begin until c. 1000 cal yr BP. After damming, four well-defined sediment pulses occurred and these are preserved in the form of distinct clay layers in most of the sediment cores. For interpreting the sediment pulses, a physically based landslide model was used to determine spatially distributed relative landslide hazard, applicable at the catchment scale. An empirical landslide-soil redistribution component was added and proved able to determine the volumes and spatial pattern of eroded and deposited soil material, sediment delivery ratio and the impact on total catchment sediment yield. Sediment volumes were calculated from the wetland cores and corresponding landslide scenarios are defined through back-analysis of modelled sediment yield output. In general, at least four major high-magnitude landslide events, both natural and intensified by forest clearance activities, occurred in the catchment upstream of Te Henga Wetland during the last c. 1000 years. The spatial distribution of modelled critical rainfall values for the catchment can be interpreted as an expression of shallow landslide hazard. The magnitude of the sediment pulses represented in the wetland can be back-calculated to critical rainfall thresholds representing a shallow landslide model scenario.en_US
dc.language.isoen
dc.publisherElsevier BVen_NZ
dc.subjectlandslide modellingen_US
dc.subjectsediment yielden_US
dc.subjectlake coresen_US
dc.subjectbenthic foraminiferaen_US
dc.subject14C datingen_US
dc.subjecttephrochronologyen_US
dc.titleReconstructing high-magnitude/low-frequency landslide events based on soil redistribution modelling and a Late-Holocene sediment record from New Zealanden_US
dc.typeJournal Articleen_US
dc.identifier.doi10.1016/j.geomorph.2005.07.008en_US
dc.relation.isPartOfGeomorphologyen_NZ
pubs.begin-page29en_NZ
pubs.elements-id31334
pubs.end-page49en_NZ
pubs.issue1-4en_NZ
pubs.volume74en_NZ


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record