MeetingOfInterest:Meeting-363: Difference between revisions
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{{CSDMS meeting details template | {{CSDMS meeting details template | ||
|MOI title meeting= | |MOI title meeting=CLAST 2019 - Climatic controls on continental erosion and sediment transport | ||
|MOI meeting detailed location description=Parque de las Ciencias | |MOI meeting detailed location description=Parque de las Ciencias | ||
|MOI meeting city= | |MOI meeting city=Juneau | ||
|MOI meeting state= | |MOI meeting state=Alaska | ||
|MOI meeting country= | |MOI meeting country=United States | ||
|MOI meeting startdate=2019/ | |MOI meeting startdate=2019/08/04 | ||
|MOI meeting enddate=2019/ | |MOI meeting enddate=2019/08/10 | ||
|MOI meeting figure=ParqueCiencias_Macroscopio2019.jpg | |MOI meeting figure=ParqueCiencias_Macroscopio2019.jpg | ||
|MOI URL conference= | |MOI URL conference=https://www.clast2019.com | ||
|MOI abstract deadline=2019/ | |MOI abstract deadline=2019/05/15 | ||
|MOI registration deadline=2019/ | |MOI registration deadline=2019/06/07 | ||
|MOI summary=Within the Topo-Europe framework, the ITN SUBITOP organises a workshop on understanding subduction zone topography through modelling of coupled shallow and deep processes. | |MOI summary=Within the Topo-Europe framework, the ITN SUBITOP organises a workshop on understanding subduction zone topography through modelling of coupled shallow and deep processes.TOPO-EUROPE promotes, coordinates and integrates national research programs on geological surface processes and their implications for continental topography and natural hazards in a coherent European network. SUBITOP is an ITN for training and career development of 15 Early Stage Researchers (ESR) in Geodynamics, Geophysics, Geology and Geomorphology. It has a scientific focus on the dynamics of continental margins where tectonic plates are recycled through subduction. '''Theme'''<br>Tectonic activity and topographic evolution are intimately linked. This is most powerfully expressed in subduction systems, where geodynamic and geomorphic processes are connected across depths and time scales from individual earthquakes to climate-driven erosion, plate deformation and slab-mantle interactions. The imprint of all these processes and their links is not only found in the surface topography of subduction systems, but also in their exposed geology and patterns of deformation with attendant hazards. Understanding of the dynamics of subduction systems is advanced by the combined reading of these geophysical, geologic and geomorphic imprints, complemented by physical and numerical modelling. | ||
TOPO-EUROPE promotes, coordinates and integrates national research programs on geological surface processes and their implications for continental topography and natural hazards in a coherent European network. SUBITOP is an ITN for training and career development of 15 Early Stage Researchers (ESR) in Geodynamics, Geophysics, Geology and Geomorphology. It has a scientific focus on the dynamics of continental margins where tectonic plates are recycled through subduction. | |||
'''Theme'''<br> | |||
Tectonic activity and topographic evolution are intimately linked. This is most powerfully expressed in subduction systems, where geodynamic and geomorphic processes are connected across depths and time scales from individual earthquakes to climate-driven erosion, plate deformation and slab-mantle interactions. The imprint of all these processes and their links is not only found in the surface topography of subduction systems, but also in their exposed geology and patterns of deformation with attendant hazards. Understanding of the dynamics of subduction systems is advanced by the combined reading of these geophysical, geologic and geomorphic imprints, complemented by physical and numerical modelling. | |||
|MOI_CSDMS_yes_no=No | |MOI_CSDMS_yes_no=No | ||
|MOI_highlight_sessions_yes_no=No | |MOI_highlight_sessions_yes_no=No | ||
Revision as of 09:46, 3 May 2019
CLAST 2019 - Climatic controls on continental erosion and sediment transport
Juneau Alaska, United States
04 - 10 August 2019
04 - 10 August 2019
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Deadlines
Abstract submission: The abstract submission deadline has passed Registration: Registration is now closed
Official website
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Within the Topo-Europe framework, the ITN SUBITOP organises a workshop on understanding subduction zone topography through modelling of coupled shallow and deep processes.TOPO-EUROPE promotes, coordinates and integrates national research programs on geological surface processes and their implications for continental topography and natural hazards in a coherent European network. SUBITOP is an ITN for training and career development of 15 Early Stage Researchers (ESR) in Geodynamics, Geophysics, Geology and Geomorphology. It has a scientific focus on the dynamics of continental margins where tectonic plates are recycled through subduction. Theme
Tectonic activity and topographic evolution are intimately linked. This is most powerfully expressed in subduction systems, where geodynamic and geomorphic processes are connected across depths and time scales from individual earthquakes to climate-driven erosion, plate deformation and slab-mantle interactions. The imprint of all these processes and their links is not only found in the surface topography of subduction systems, but also in their exposed geology and patterns of deformation with attendant hazards. Understanding of the dynamics of subduction systems is advanced by the combined reading of these geophysical, geologic and geomorphic imprints, complemented by physical and numerical modelling.
Tectonic activity and topographic evolution are intimately linked. This is most powerfully expressed in subduction systems, where geodynamic and geomorphic processes are connected across depths and time scales from individual earthquakes to climate-driven erosion, plate deformation and slab-mantle interactions. The imprint of all these processes and their links is not only found in the surface topography of subduction systems, but also in their exposed geology and patterns of deformation with attendant hazards. Understanding of the dynamics of subduction systems is advanced by the combined reading of these geophysical, geologic and geomorphic imprints, complemented by physical and numerical modelling.
Of interest for: Terrestrial Working Group Geodynamics Focus Research Group
