Ultraslow spreading mid-ocean ridges

At mid-ocean ridges, the lithospheric plates move apart at rates of about 5-150 mm/year and new oceanic lithosphere is continuously formed. At low spreading rates of less than 20 mm/year, this engine stutters. Very little melt is formed and it has difficulty in making its way to the ocean floor through a cold, thick lithosphere. Therefore, the formation process of new ocean lithosphere differs at ultraslow spreading ridges from all other ocean basins. Ultraslow ridges represent a separate category of mid-ocean ridges, accounting for about 15% of the total length of mid-ocean ridges worldwide. Since ultraslow ridges are located in the Arctic Ocean and the stormy Southwest Indian Ocean and are therefore fairly difficult to reach, the spreading processes of this distinct class of mid-ocean ridges are still poorly understood. 

In various research projects we are investigating the active spreading processes based on the seismic activity of the Arctic Ridge System. We are particularly interested in the interaction of ocean and lithosphere at the enigmatic hydrothermal vents of the Arctic Ridge system.

In the project KNIPAS "Knipovich Ridge Passive Seismic Experiment" we recorded and analyzed earthquake activity between two volcanic centres along an entire ultraslow ridge segment.

How do the hydrothermal fields of Aurora, Jotul and Loki's Castle work? We are looking for answers in extensive microearthquake data sets.

We are also involved in other projects along slow and ultraslow spreading ridges.