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Landforms from the quaternary glaciation of Papua New Guinea: an overview of ice extent during the last glacial maximum
School of Geography and Environmental Science, Monash University.
School of Geography and Environmental Science, Monash University.
2004 (English)In: Developments in Quaternary Science, ISSN 1571-0866, Vol. 2, no Part C, p. 313-319Article in journal (Refereed) Published
Abstract [en]

Documentation of glacial landforms of Papua New Guinea is dominated by accounts of landscapes that are supported by chronologies assembled during biostratigraphical studies of peat cores showing that glacial landscape reconstruction will refer to the Last Glacial Stage. The steep terrain ensured that the scale of the air photographs used in these studies would vary all over the stereographic models formed for landscape interpretation. Here, in the form of annotated ortho-rectified (i.e. scale-consistent) satellite images, a summary of the maps found in the literature is presented, together with the results of simple spatial query designed to refine the accuracy of previously-estimated Last Glacial Maximum (LGM) ice extents

Place, publisher, year, edition, pages
2004. Vol. 2, no Part C, p. 313-319
National Category
Geochemistry
Research subject
Applied Geology
Identifiers
URN: urn:nbn:se:ltu:diva-8074DOI: 10.1016/S1571-0866(04)80136-2Scopus ID: 2-s2.0-77956775655Local ID: 68308e10-cd29-11df-a707-000ea68e967bOAI: oai:DiVA.org:ltu-8074DiVA, id: diva2:980964
Note
Validerad; 2004; 20101001 (andbra)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-07-10Bibliographically approved

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Lundberg, Christian

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