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’ by Sigrid Østmo da Costa’Using large-scale patterns and morphology of subglacial meltwater corridors to gain insight into the spatial organisation, formation and evolution of meltwater drainage beneath ice sheets’ by Emma Lewington’The Kassen and Håkåneset rock slope instabilities along fjord lakes in Telemark show large postglacial gravitational strain but no present day deformation, Southern Norway The Kassen and Håkåneset rock slope instabilities along fjord lakes in Telemark show large postglacial gravitational strain but no present day deformation, Southern Norway’ by Kaja Krogh’An automated cryogenic magnetometer at the Geological Survey of Norway for natural remanent magnetization and rock magnetism: A case study of North-East Atlantic continental margin sediments’ by Martin Klug’Stratigraphy and sedimentary architecture of polder fills along the North Frisian Wadden Sea (southern North Sea) – potential archives of sea-level and climate variability (project SEASTORM) ’ by Amalie Cordua Session 1.1.Hotspots and intraplate magmas: Mantle sources, magmatic processes and metasomatism.Cancellation of participation (a written request is mandatory) Pre-registered participants who are unable to attend the meeting will have their paid fees reimbursed less a processing fee of DKK 400 provided written notice of non-attendance is received by the Meeting Secretariat before 10 December 2017. If cancellation is made after this date no refund of the fee can be expected.- Registration at Geocenter Copenhagen at Øster Voldgade 10, 1350 (Central Copenhagen) - Geology Walking Tour around Copenhagen for registered participants (meeting point at Institute for Geoscience at Øster Voldgade 10, 1350) Groundwater transport in cold, changing climates: theory, experiments, models Groundwater – surface water interaction; chemical and quantitative impacts on rivers, lakes, wetlands, fjords and coastal areas.This session invites contributions that explore the mantle geochemistry, petrology and dynamics of intraplate volcanism both in oceanic and continental settings.

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He graduated from Shimane University in 1994, and received a master’s degree from Kanazawa University in 1996, then a Ph. In September 2015, he began as a professor at the Center for Northeast Asian Studies at Tohoku University.

Conveners: Nina Søager (University of Copenhagen), Valentin Troll (Uppsala University), Abi Barker (Uppsala University) Session 1.2.

Volcanism in the North Atlantic, from breakup to current time The opening of the North Atlantic Ocean is a geological event that occurred over millions of years, during which the supercontinent Pangea broke up.

A., A bag of sand from the ice-concealed, 31 km large Hiawatha crater in North-West Greenland: samples of the impact plume, ejecta blanket and crater floor from a recent meteorite impact through the Greenland ice sheet All Posters will be present at Glassalen during the entire conference.

All the ones with blue-green mark on the left are in the competition for the Best Student Poster Award.

He graduated from Shimane University in 1994, and received a master’s degree from Kanazawa University in 1996, then a Ph. In September 2015, he began as a professor at the Center for Northeast Asian Studies at Tohoku University.

Conveners: Nina Søager (University of Copenhagen), Valentin Troll (Uppsala University), Abi Barker (Uppsala University) Session 1.2.

Volcanism in the North Atlantic, from breakup to current time The opening of the North Atlantic Ocean is a geological event that occurred over millions of years, during which the supercontinent Pangea broke up.

A., A bag of sand from the ice-concealed, 31 km large Hiawatha crater in North-West Greenland: samples of the impact plume, ejecta blanket and crater floor from a recent meteorite impact through the Greenland ice sheet All Posters will be present at Glassalen during the entire conference.

All the ones with blue-green mark on the left are in the competition for the Best Student Poster Award.

The strength of his research lies in combining detailed fieldwork and geological observations with quantitative petrological and geochronological approaches aimed at understanding the geodynamic processes at convergent plate boundaries—from mineral equilibrium/kinetics scale to plate tectonic scale.