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- W1520093721 endingPage "768" @default.
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- W1520093721 abstract "The reconstruction of glacier and ice-sheet dynamics over complete glacial cycles (paleoglaciology) can be facilitated by basin-wide assessments of glacial sediment and landform distributions, informed by modern glacial landsystem analogs. Significant developments in interpreting ancient glaciated landscapes have highlighted complex but coherent patterns of glacier activity over much of the last glacial cycle. These paleoglaciological reconstructions are being increasingly linked with regional and global climatic and oceanographic changes. This article summarizes the range of glacial landforms employed in Quaternary paleoglaciology by using a landsystems approach, thereby summarizing the sediment–landform associations that are characteristic of particular topographic and environmental settings. Landforms are introduced within their characteristic process–form domains, including the subglacial environment, ice-marginal and supraglacial settings, subaqueous environments, and mountainous terrain." @default.
- W1520093721 created "2016-06-24" @default.
- W1520093721 creator A5028501880 @default.
- W1520093721 creator A5048498343 @default.
- W1520093721 date "2013-01-01" @default.
- W1520093721 modified "2023-09-23" @default.
- W1520093721 title "GLACIAL LANDFORMS | Introduction" @default.
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