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Physiography and late structural history of the area drained by the streams flowing into porirua harbour, near Wellington, New Zealand

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dc.contributor.authorQuennell, Albert Mathieson
dc.date.accessioned2012-01-31T00:10:37Z
dc.date.accessioned2022-11-01T00:18:46Z
dc.date.available2012-01-31T00:10:37Z
dc.date.available2022-11-01T00:18:46Z
dc.date.copyright1938
dc.date.issued1938
dc.description.abstractThe area under discussion embraces the drainage basin of the streams flowing into Porirua Harbour, which is situated on the west coast of the North Island of New Zealand about eighteen miles north-east of Cape Terawhiti, the most south-westerly point of the Island. Some other localities are described and discussed, where necessary for the elucidation of problems connected with the area. The area covered In the discussion is approximately sixty square miles in extent.en_NZ
dc.formatpdfen_NZ
dc.identifier.urihttps://ir.wgtn.ac.nz/handle/123456789/27416
dc.languageen_NZ
dc.language.isoen_NZ
dc.publisherTe Herenga Waka—Victoria University of Wellingtonen_NZ
dc.rights.holderAll rights, except those explicitly waived, are held by the Authoren_NZ
dc.rights.licenseAuthor Retains Copyrighten_NZ
dc.rights.urihttps://www.wgtn.ac.nz/library/about-us/policies-and-strategies/copyright-for-the-researcharchive
dc.subjectGeologyen_NZ
dc.subjectPoriruaen_NZ
dc.titlePhysiography and late structural history of the area drained by the streams flowing into porirua harbour, near Wellington, New Zealanden_NZ
dc.typeTexten_NZ
thesis.degree.grantorTe Herenga Waka—Victoria University of Wellingtonen_NZ
thesis.degree.levelMastersen_NZ
vuwschema.type.vuwAwarded Research Masters Thesisen_NZ

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