Publication:
Mass movement in Tangoio conservation reserve northern Hawkes Bay

dc.contributor.authorEyles, R.J.
dc.date.accessioned2015-02-12T03:54:02Z
dc.date.available2015-02-12T03:54:02Z
dc.date.issued1971
dc.description.abstractIn a random sample of 52 valley-side profiles at Tangoio, mass movements are shown to occur preferentially on profiles with a northerly aspect, which are long, or steeply sloping. Detailed measurements of 27 debris slide and two slump scars dating from a storm in May 1971 enable an estimate of the rate of erosion of loess and volcanic ash from valley-sides to be made. Valley-side slopes are changing from a convexo-concave equilibrium form under the original forest towards a new, more rectilinear equilibrium form under grass.en_NZ
dc.format.mimetypeapplication/pdf
dc.identifier.citationEyles, R.J. (1971). Mass movement in Tangoio conservation reserve northern Hawkes Bay. Earth Science Journal, 5(2), 79-91.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/9187
dc.language.isoenen_NZ
dc.publisherWaikato Geological Society, The University of Waikatoen_NZ
dc.relation.ispartofseriesEarth Science Journalen_NZ
dc.rights© 1971 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.titleMass movement in Tangoio conservation reserve northern Hawkes Bayen_NZ
dc.typeJournal Articleen_NZ
dspace.entity.typePublication

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