At the northern end of our travels we are looking at the
Bear Island Fan. This is one of the largest packages of fan sediments in the
world. It extends from the continental shelf just south of Bear Island
westwards to the Mid-Atlantic Ridge (MAR). We wanted to see if any of the
debris flows that make up the fan reach the centre of the MAR. This gave us an
opportunity to survey along this dramatic structure to see if there was a
suitable site to sample. First as we approached the ridge we could see on the
3.5kHz pinger records blocks of rock protruding through the well layered
sediments. The multibeam showed that these blocks were parallel to the MAR and
increasing in height and extent as we moved towards to the actual ridge.
Then we reached the ridge itself. As we steamed along its
axis with Pelagia’s starboard side above
the European Plate and its port side above the American Plate the multibeam
display was a confirmation of all those sketch diagrams on plate tectonics explaining
the formation of oceanic crust at spreading centres, with each line of multibeam
data added to the swath showed ridges parallel to the axis or evidence of
volcanic activity. The ridge exhibits sudden large changes in bathymetry that makes
following the seabed on the 3.5kHz pinger involve frequent changes of the display
offset. It showed the rocky seafloor but we could see no thick sequences of
sediments so we moved away to investigate the debris flows at the edge of the
Bear Island Fan only a short distance to the east where we recovered a 10m long
core with a very good record of the Bear Island Fan.
Image from the Swath multibeam onboard the RV Pelagia of the Mid-Atlantic Ridge. |
David Long