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dc.contributor.authorLowe, David J.en_NZ
dc.contributor.authorGreen, John D.en_NZ
dc.contributor.editorViner, A.B.
dc.date.accessioned2016-07-22T04:00:37Z
dc.date.available1987en_NZ
dc.date.available2016-07-22T04:00:37Z
dc.date.issued1987en_NZ
dc.identifier.citationLowe, D. J., & Green, J. D. (1987). Origins and development of the lakes. In A. B. Viner (Ed.), Inland Waters of New Zealand (pp. 1–64). Wellington: New Zealand Department of Scientific and Industrial Research.en
dc.identifier.isbn0-477-06799-9en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/10555
dc.description.abstractBecause of a turbulent and complex recent geological history, New Zealand has an impressively diverse and dynamic landscape, and a correspondingly wide array of lake types, within a small land area (Irwin 1975a; Soons & Selby 1982;). The development of such an active geological environment in New Zealand has been governed largely by its location athwart the Australian and Pacific plate boundary, and its maritime mid-latitude position has made it particularly sensitive to the climatic fluctations and associated glaciations and sea level changes of the Quaternary Period (Suggate et al. 1978). At present, the rates of uplift and erosion of mountainous areas are among the fastest in the world. Earthquakes are common, and volcanism has characterised much of the North Island during the Quaternary with numerous volcanoes active in the last few thousand years. Large, explosive caldera volcanoes in central North Island have erupted repeatedly over the last million years, producing voluminous amounts of lava and widespread pyroclastic deposits. The landforms, soils and lakes are thus typically youthful, almost all being younger than two million years; indeed, much of the landscape is of late Pleistocene and Holocene age, and is still actively developing (Pillans et al. 1982). Our purpose in this chapter is to outline the relationship between these often violent and spectacular geological processes which have led to the formation and development of the various lake types in New Zealand. Against this background we describe the classification and distribution of the main lake types, their ages and mechanisms of formation. We also comment on lake sedimentation patterns, palaeolimnological studies, and on features of lake bathymetry and morphology.
dc.format.extent16en_NZ
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherNew Zealand Department of Scientific and Industrial Researchen_NZ
dc.rightsThis article is published in the book: Inland waters of New Zealand. © 1987 Crown copyright.
dc.titleOrigins and development of the lakesen_NZ
dc.typeChapter in Book
dc.relation.isPartOfInland Waters of New Zealanden_NZ
pubs.begin-page1
pubs.elements-id115354
pubs.end-page64
pubs.place-of-publicationWellingtonen_NZ
pubs.publication-statusPublisheden_NZ
pubs.volume241en_NZ
uow.identifier.chapter-no1


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