Supraglacial Re-Sedimentation from Melt-Water Streams on to Snow Overlying Glacier Ice, Sylgjujökull, West Vatnajökull, Iceland

Abstract Sediment deposition on to snow overlying glacier ice occurs in a marginal zone extending 200–300 m up-glacier from the terminus of Sylgjujökull. Debris on ice above the marginal snow zone comes from debris-rich layers, and 85% of this debris falls between 1 and 4 ϕ , the characteristic grai...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Dowdeswell, Julian A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1982
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000011709
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011709