Scheduled Cruises in 2004
Summary of a cruise on margins research (UK.042)
Agadir Basin, Morocco, NW Africa ; SME21
& SME33
Charles Darwin
26th October 2004
from ; Lisbon, PORTUGAL
19th November 2004
to ; Madeira, PORTUGAL
26 Days
Russell Wynn
Southampton
Oceanography Centre (SOC)
Dr Bryan
Cronin
classroom@sea.
See also the UK-TAPS Group website - here
Fig - The Agadir
Basin, off Morocco, NW Africa.
The main aim of the cruise is to take sediment samples (cores) from the
deep Agadir Canyon and Basin.
The water is over 4 km deep in this region, and the work area is
several hundred kilometres from the
Moroccan coast to the east and the volcanic Canary Islands to the
south.
However, earlier investigations in this areas have shown that the
seafloor sediments contain
Moroccan beach sands, volcanic lava fragments from Tenerife, and even
pieces of wood!
This material was transported down to the deep sea by giant underwater
avalanches
(composed of a turbulent mixture of water, sand and mud), that
originate as landslides in shallower
water close to land.
These underwater avalanches then travel downslope at high speed through
canyons and channels
until they reach the flat basin floor. Most of their sand and mud is
then dumped, smothering
huge areas of seafloor and destroying all life.
By studying the deposits left behind by these catastrophic events,
scientists can work out
where they come from, how often they occur, and whether they are
capable of generating
potentially damaging tidal waves that could effect coastal towns and
villages in the region.
They can also see how quickly deep-sea organisms can re-colonise the
seafloor after being exterminated.
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