Dynamics of the Ocean Floor

The Research Division Dynamics of the Ocean Floor has two Research Units: Magmatic and Hydrothermal Systems and Marine Geodynamics.

Contact

Head of the Research Division:

Prof. Dr. Heidrun Kopp
GEOMAR Helmholtz Centre for Ocean Research Kiel
East shore campus
Wischhofstr. 1-3 
D-24148 Kiel
Germany

Phone: +49-431-600-2334
Fax: +49-431-600-2922
e-mail: hkopp(at)geomar.de

Personal Assistent/Office Management:
Jasmin Mögeltönder
Phone: +49-431-600-2271
e-mail: jmoegeltoender(at)geomar.de

Anne Völsch
Phone: +49-431-2271
e-mail: avoelsch(at)geomar.de

Publications

Overview

The research focus is on the geological-geophysical survey of the ocean floor and the margins of the ocean basins. The core topics include processes of formation, development, alteration and subduction of the oceanic lithosphere and the associated effects on the environment, for example on the climate and the emergence of natural hazards.

These research topics are addressed in three geotectonic areas:

  • Divergent plate margins: Formation of the ocean floor and the ocean basins
  • Convergent plate margins: the subduction engine
  • Tectonic and magmatic processes in the intraplate zone: Conversion of oceanic plates

Significant research emphasis is placed on:

  • Marine natural hazards: earthquakes, volcanoes, slope stability, submarine landslides, and tsunamis
  • Seafloor resources: Gas hydrates and polymetallic massive sulphides
  • Introduction of volatiles into the atmosphere and hydrosphere

RD4 News

Today's Galapagos islands at the volcanic Galapagos-Hotspot are only about four four million years old. Traces of older eruptions have been found in cores obtained off the coast of Costa Rica. Image reproduced from the GEBCO world map 2014, www.gebco.net
01.06.2015

Highly Explosive Volcanism at Galapagos

International team of volcanologists presents new findings on the eruption history

more
Map of the Hawaiian Emporer bend.
27.04.2015

Composers provide explanation for Hawaiian Emporer bend

International team of researchers finds evidence of large-scale tectonic changes in the Pacific taking place 50 million years ago

more