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dc.contributor.authorTonkin, Philip J.
dc.date.accessioned2015-02-03T20:01:19Z
dc.date.available2015-02-03T20:01:19Z
dc.date.issued1967
dc.identifier.citationTonkin, P.J. (1967). Note on the occurrence of Taupo pumice in the Hamilton basin. Earth Science Journal, 1(1), 31-32en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/9102
dc.description.abstractThe presence of a thin layer of pumice lapilli and ash close to the surface of the Rukuhia and Moanatuatua peat bogs was recorded by Grange and Taylor (1939). Since this time a similar band of pumice has been noted in many of the other peat areas in the Hamilton basin. In the undeveloped fibrous peats of the Woodlands bog a layer of pumice lapilli 2 to 3 inches thick occurs at a depth of 18 to 20 inches from the surface. This is similar to the observations of Grange and Taylor. In the more loamy peats the pumice layer is predominantly fine ash and any lapilli present are extremely weathered and crush easily. In the fibrous peats it is thought that the fine ash that fell on the bog surface soon dispersed in the loose network of dead material, whereas the lapilli were of sufficient size to be trapped. In the loamy peats more active weathering took place in an acid environment as the organic matter was breaking down. This made the lapilli very fragile, so with drainage and compaction of the peat the lapilli were very soon crushed to fine ash size.en_NZ
dc.format.mimetypeapplication/pdf
dc.publisherWaikato Geological Society, The University of Waikatoen_NZ
dc.relation.ispartofseriesEarth Science Journalen_NZ
dc.rights© 1967 Waikato Geological Society, The University of Waikato. All items in Research Commons are provided only to permit fair dealing for the purposes of research or private study. They are protected by copyright with all rights reserved unless otherwise indicated.en_NZ
dc.subjectHamilton basinen_NZ
dc.titleNote on the occurrence of Taupo pumice in the Hamilton basinen_NZ
dc.typeJournal Articleen_NZ


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