Self-formed bedrock channels
- Author
- WOBUS, Cameron W1 ; TUCKER, Gregory E2 ; ANDERSON, Robert S3
[1] Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, United States
[2] Department of Geological Sciences and Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, United States
[3] Department of Geological Sciences and Institute for Arctic and Alpine Research, University of Colorado, Boulder, Colorado, United States - Source
Geophysical research letters. 2006, Vol 33, Num 18 ; L18408.1-L18406.6 ; ref : 20 ref
- CODEN
- GPRLAJ
- ISSN
- 0094-8276
- Scientific domain
- Astronomy earth cosmic environment; Geophysics; Climatology, meteorology; Oceanography
- Publisher
- American Geophysical Union, Washington, DC
- Publication country
- United States
- Document type
- Article
- Language
- English
- Keyword (fr)
- Apport sédiment Bedrock Chenal Climat Coupe transversale Débit Fluidalité Loi puissance Modèle Modélisation Paysage Prospection Section efficace Stratégie Surrection Taux érosion Tectonique Versant
- Keyword (en)
- sediment supply bedrock channels climate cross sections discharge flow structures Power law models Modeling landscapes exploration Cross section (collision) strategy uplifts erosion rates tectonics slopes
- Keyword (es)
- Roca firme Canal Clima Gasto Fluidal Ley poder Modelo Modelización Paisaje Prospección Sección eficaz Estrategia Proporción material erosionado Tectónico Declive
- Classification
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 18232231
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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