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A study of roundness of wind-blown sands from Hungary and the Canadian great plains.

The degree of roundness of sand grains, comprising relatively insoluble minerals such as quartz and feldspar, within a specific size range increases with the distance of eolian transport. Roundness indices based on visual recognition and counting of four grain types were used to study sands from the Alfold in Hungary and the Great Sand Hills in Saskatchewan. The Saskatchewan sand showed a significant increase in roundness within about five miles. All the sands in the sand plateau of the Alfold are eolian and increase in roundness with the distance from their source (the Duna (Danube) Valley).

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.113368
Date January 1961
CreatorsDavid, Peter. P.
ContributorsElson, J. (Supervisor)
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageMaster of Science. (Department of Earth Sciences.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

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