Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Ed Self"'
Autor:
James D. Kirkham, Kelly A. Hogan, Robert D. Larter, Neil S. Arnold, Jeremy C. Ely, Chris D. Clark, Ed Self, Ken Games, Mads Huuse, Margaret A. Stewart, Dag Ottesen, Julian A. Dowdeswell
The geological record of landforms and sediments produced beneath deglaciating ice sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed by meltwater erosion of sediments (tunnel valleys) are widespread in former
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::373a0a02bdcf2b3cb7957b3b62708cc6
Autor:
Robert D Larter, Kelly A. Hogan, Margaret Stewart, Neil Arnold, Ken Games, Ed Self, Jeremy C. Ely, James D. Kirkham, Mads Huuse, Julian A. Dowdeswell, Dag Ottesen
The geological record of landforms produced beneath deglaciating ice sheets offers insights into otherwise inaccessible subglacial processes. Large subglacial channels formed by meltwater erosion of sediments (tunnel valleys) are widespread in former
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac6938e672e7ae5b463cf69e74a747f3
https://doi.org/10.5194/egusphere-egu21-2183
https://doi.org/10.5194/egusphere-egu21-2183
Autor:
Robert D Larter, Ed Self, Ken Games, Neil Arnold, Mads Huuse, Julian A. Dowdeswell, Dag Ottesen, Margaret Stewart, James D. Kirkham, Kelly A. Hogan
Landforms produced beneath former ice sheets offer insights into inaccessible subglacial processes and present analogues for how current ice masses may evolve in a warming climate. Large subglacial channels cut by meltwater erosion (tunnel valleys [T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::28f9a133292ac8862e6816e0aab177bd
https://www.repository.cam.ac.uk/handle/1810/327768
https://www.repository.cam.ac.uk/handle/1810/327768
Autor:
Kelly A. Hogan, Robert D Larter, Julian A. Dowdeswell, Mads Huuse, Ken Games, Dag Ottesen, Ed Self, Neil Arnold, Margaret Stewart, James D. Kirkham
Tunnel valleys are large (kilometres wide, hundreds of metres deep) channels incised into bedrock and soft sediments by the action of pressurised subglacial meltwater. Discovered over a century ago, they are common across large swathes of North-West
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23ff432566e1ad241470486d6faa3348
https://doi.org/10.5194/egusphere-egu2020-118
https://doi.org/10.5194/egusphere-egu2020-118