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The effects of entrained debris on the basal sliding stability of a glacier

Author
ZOET, L. K1 2 ; CARPENTER, B3 ; SCUDERI, M1 ; ALLEY, R. B1 ; ANANDAKRISHNAN, S1 ; MARONE, C1 ; JACKSON, M4
[1] Department of Geoscience, Penn State University, University Park, Pennsylvania, United States
[2] Department of Geologic and Atmospheric Sciences, Iowa State University, Ames, Iowa, United States
[3] HP-HT Lab, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
[4] Hydrology Department Norwegian Water Resources and Energy Directorate, Oslo, Norway
Source

Journal of geophysical research. Earth surface. 2013, Vol 118, Num 2, pp 656-666, 11 p ; ref : 1 p.1/4

ISSNNV
2169-9003
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
Wiley, Hoboken, NJ
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Bedrock Claste Comportement Contrôle Débris Eau fonte Effet Etude expérimentale Frottement Glace Glacier rocheux Glissement saccadé Interface Matière fondue Mouvement Production chaleur Rapides Rapport Stabilité Substrat Vitesse
Keyword (en)
bedrock clasts behavior controls debris meltwater effects experimental studies friction ice rock glaciers stick-slip interfaces melts movement heat production rapids report stability substrates velocity
Keyword (es)
Roca firme Clasto Pedazos Agua deshielo Hielo Movimiento a tirones Interfase Producto fundido Producción calor Estabilidad Velocidad
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
27674322

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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