Quaternary geomorphology, stratigraphy, and paleoclimate of the central Southern Alps, South Island

dc.contributor.authorAlmond, Peter C.
dc.contributor.authorBarrell, D.
dc.contributor.authorHyatt, O.
dc.contributor.authorRother, H.
dc.contributor.authorShulmeister, J.
dc.contributor.authorVandergoes, M.
dc.date.accessioned2012-12-14T03:49:04Z
dc.date.issued2007
dc.description.abstractOn our first day we leave Christchurch and travel inland to the eastern front range of the Southern Alps, venturing into the Rakaia valley. Here we will see spectacular examples of glacial landforms, glacial sedimentology, and post glacial valley modification. After leaving the Rakaia Valley we follow the foot of ranges southwards to the McKenzie Basin, a tectonic depression adjacent to the highest peaks in the Southern Alps. Twizel is our stop for the night. Day 2, we backtrack slightly and head up the southern flank of Lake Pukaki, one of the large finger lakes described above, to Mt Cook village, seeing glacial features ranging from Last Glacial Maximum to latest Holocene in age, as well as present-day glaciers. From Mt Cook village we retrace our steps to Twizel and continue south to the driest and most continental region of New Zealand, Central Otago. We stay on the shores of Lake Wanaka for the night of Day 2. Day 3 takes us from the dry climates of Central Otago to the wet, forest cloaked landscape of the West Coast via the Haast Pass over the Southern Alps. This day involves soils, Holocene coastal geomorphology, marine terraces and late glacial moraines. The day ends in the township of Franz Josef. Day 4 starts with a plane flight for those with the inclination or a trip up to see the Franz Josef glacier. Afterwards we travel to Okarito Bog, the site of a splendid pollen record spanning the complete last glacial cycle, then head north to Hokitika. On the way we stop to discuss last glacial maximum moraines in the Poerua valley, and the effects of a recent large landslide on the landscape and people of the valley. The area around Hokitika is the focus of the next day when we review the classic glacial geomorphology of the Hokitika-Taramakau systems. The final part of the day takes us to Punakaiki on the western flanks of the Paparoa Range. On day 6 we continue north, stopping briefly near Westport to discuss a well studied peat section on a marine terrace of Cape Foulwind, then head through the Buller Gorge to the Inangahua Valley. We then turn south again to re-cross the Southern Alps over the Lewis Pass. Our final stop of the tour before Christchurch is in the Hope Valley.en
dc.format.extent1-71en
dc.identifier.citation2007, pp. 1 - 71
dc.identifier.citation2007, pp. 1 - 71
dc.identifier.citation2007, pp. 1 - 71
dc.identifier.citation2007, pp. 1 - 71
dc.identifier.isbn978-0-86476-189-7en
dc.identifier.urihttps://hdl.handle.net/10182/5112
dc.language.isoen
dc.publisherLincoln University.
dc.relationThe original publication is available from - Lincoln University.en
dc.relation.hasversionThe original publication is available from Lincoln University.
dc.relation.hasversionThe original publication is available from Lincoln University.
dc.rightsCopyright © The Authors.
dc.subjectSouthern Alpsen
dc.subjectgeomorphologyen
dc.subjectstratigraphyen
dc.subjectpaleoclimateen
dc.subjectquaternaryen
dc.titleQuaternary geomorphology, stratigraphy, and paleoclimate of the central Southern Alps, South Islanden
dc.typeOther
lu.contributor.unitLincoln University
lu.contributor.unitFaculty of Agriculture and Life Sciences
lu.contributor.unitDepartment of Soil and Physical Sciences
lu.identifier.orcid0000-0003-4203-1529
pubs.confidentialfalseen
pubs.notesXVII INQUA Conference 2007, Post Conference Field Trip Guide.en
pubs.publication-statusPublisheden
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