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dc.contributor.authorForce, Eric R.
dc.contributor.authorForce, Lucy M.
dc.contributor.authorThyne, Martin L.
dc.date.accessioned2015-02-11T01:51:43Z
dc.date.available2015-02-11T01:51:43Z
dc.date.issued1970
dc.identifier.citationForce, E.R., Force, L.M. & Thyne, M.L. (1970). Quaternary warping at Gorge Saddle, western Southland. Earth Science Journal, 4(2), 141-144.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/9168
dc.description.abstractGorge Saddle is one low point on a drainage divide between Fiordland and the Southland Plain. Eastward sloping Quaternary terraces east of the divide and westward sloping terraces to the west contain granitic pebbles which could have been derived only from the west. This suggests doming at the present divide concurrent with transport from the west.en_NZ
dc.format.mimetypeapplication/pdf
dc.publisherWaikato Geological Society, The University of Waikatoen_NZ
dc.relation.ispartofseriesEarth Science Journalen_NZ
dc.rights© 1970 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.titleQuaternary warping at Gorge Saddle, western Southlanden_NZ
dc.typeJournal Articleen_NZ


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