Fluvial responses to environmental change in the North Island, New Zealand, during the past c. 30 ka recorded in river terrace sequences: A review and model for river behaviour
This paper presents a systematic review and correlation of river terraces identified in 44 river catchments in the North Island, New Zealand, to assess river behaviour over the last c. 30 000 yr. This provides a comprehensive foundation from which to assess controls on river dynamics over this criti...
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Veröffentlicht in: | New Zealand journal of geology and geophysics 2007-06, Vol.50 (2), p.101-116 |
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creator | Clement, Alastair J.H. Fuller, Ian C. |
description | This paper presents a systematic review and correlation of river terraces identified in 44 river catchments in the North Island, New Zealand, to assess river behaviour over the last c. 30 000 yr. This provides a comprehensive foundation from which to assess controls on river dynamics over this critical period of landscape development from the last glacial through to the present interglacial. From this review, an integrated framework for elucidating fluvial responses to environmental change is proposed. Sensitivity of river systems to climate change is variable over this time-scale. Substantial sediment inputs to valley floors during the last glacial reduced sensitivity to subtle climatic shifts. Sensitivity increased during the Holocene, with terraces forming in response to episodes of storminess. Tectonics and volcanic activity may both override climatic forcing to cause either cutting or filling of the valley floor. |
doi_str_mv | 10.1080/00288300709509824 |
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This provides a comprehensive foundation from which to assess controls on river dynamics over this critical period of landscape development from the last glacial through to the present interglacial. From this review, an integrated framework for elucidating fluvial responses to environmental change is proposed. Sensitivity of river systems to climate change is variable over this time-scale. Substantial sediment inputs to valley floors during the last glacial reduced sensitivity to subtle climatic shifts. Sensitivity increased during the Holocene, with terraces forming in response to episodes of storminess. Tectonics and volcanic activity may both override climatic forcing to cause either cutting or filling of the valley floor.</description><subject>aggradation</subject><subject>climate</subject><subject>degradation</subject><subject>river terrace</subject><subject>tectonics</subject><subject>volcanism</subject><issn>0028-8306</issn><issn>1175-8791</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNqFkMFu1DAQhi0EEkvhAbjNA5BiJ944QVyqikKlqr3AhUs0sSddQ9Zext6UvhWPiLfbW4U4jUbzf9-MRoi3Sp4q2cn3UtZd10hpZL-WfVfrZ2KllFlXnenVc7E6zKsSaF-KVyn9KG2re7USfy7m_eJxBqa0iyFRghyBwuI5hi2FXEZ2g-GWwAfIG4LryHkDl2nG4N7BNd3Bd8Jj4_bsw-1Daocpgz2FRsJPLHIb2ZE7ONgvxJCJGS1Bol97CpbSBzgrscUXX3HBNjqaYYr8mB9pg4uPe34tXkw4J3rzWE_Et4tPX8-_VFc3ny_Pz64q1KrOVYeNM50zrqml1n1tW4OTG13btLpRNZFz2sla96MhjeMkrVHjRG6t3IhrouZEqKPXckyJaRp27LfI94OSw-Hlw5OXF8YcGR_K5Vu8izy7IeP9HHliDNanp9SQf-dCfvwv2fx78V_lVZyN</recordid><startdate>20070601</startdate><enddate>20070601</enddate><creator>Clement, Alastair J.H.</creator><creator>Fuller, Ian C.</creator><general>Taylor & Francis Group</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20070601</creationdate><title>Fluvial responses to environmental change in the North Island, New Zealand, during the past c. 30 ka recorded in river terrace sequences: A review and model for river behaviour</title><author>Clement, Alastair J.H. ; Fuller, Ian C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a412t-8a3d78d7d3204492c67afdbd6364312eedd4d0249b7e4abf0c71bfed51dba5ee3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>aggradation</topic><topic>climate</topic><topic>degradation</topic><topic>river terrace</topic><topic>tectonics</topic><topic>volcanism</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Clement, Alastair J.H.</creatorcontrib><creatorcontrib>Fuller, Ian C.</creatorcontrib><collection>CrossRef</collection><jtitle>New Zealand journal of geology and geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Clement, Alastair J.H.</au><au>Fuller, Ian C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Fluvial responses to environmental change in the North Island, New Zealand, during the past c. 30 ka recorded in river terrace sequences: A review and model for river behaviour</atitle><jtitle>New Zealand journal of geology and geophysics</jtitle><date>2007-06-01</date><risdate>2007</risdate><volume>50</volume><issue>2</issue><spage>101</spage><epage>116</epage><pages>101-116</pages><issn>0028-8306</issn><eissn>1175-8791</eissn><abstract>This paper presents a systematic review and correlation of river terraces identified in 44 river catchments in the North Island, New Zealand, to assess river behaviour over the last c. 30 000 yr. 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source | Royal Society of New Zealand Open Access Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
subjects | aggradation climate degradation river terrace tectonics volcanism |
title | Fluvial responses to environmental change in the North Island, New Zealand, during the past c. 30 ka recorded in river terrace sequences: A review and model for river behaviour |
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