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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.author Quennell, Albert Mathieson
dc.date.accessioned 2012-01-31T00:10:37Z
dc.date.accessioned 2022-11-01T00:18:46Z
dc.date.available 2012-01-31T00:10:37Z
dc.date.available 2022-11-01T00:18:46Z
dc.date.copyright 1938
dc.date.issued 1938
dc.identifier.uri https://ir.wgtn.ac.nz/handle/123456789/27416
dc.description.abstract The 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.format pdf en_NZ
dc.language en_NZ
dc.language.iso en_NZ
dc.publisher Te Herenga Waka—Victoria University of Wellington en_NZ
dc.title Physiography and late structural history of the area drained by the streams flowing into porirua harbour, near Wellington, New Zealand en_NZ
dc.type Text en_NZ
vuwschema.type.vuw Awarded Research Masters Thesis en_NZ
thesis.degree.grantor Te Herenga Waka—Victoria University of Wellington en_NZ
thesis.degree.level Masters en_NZ


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