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Expedition
to the Mariana forearc
Mar.
23 - May 4, 2003
Days
8 & 9, March 30 & 31
(click
on any image for the larger version)
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Days
8 and 9: BLUE MUD!!!
Day
8: Big Blue Seamount—we arrived early and set the transponders.
The DSL-120 was deployed using Medea
(from Jason 2) as the weight in hope of solving the problems of
the cable twisting and tangling. Medea communicates with the control
van and so does the DSL-120 so the system had to be electrically
reconfigured before deployment. Once launched, there were unexpected
electrical complications, so it was back onboard for Medea and the
DSL-120. By 0930 we were preparing a gravity core of the summit
of Big Blue. I asked Chris
Moser, the coring specialist, why there was a plastic bucket
lid tied near the end of the core pipe. He explained that this “high
tech” device would, hopefully, break free when the core pipe penetrated
the mud. Later, when we come back to this site with Jason 2, we
will see the bucket lid marking the location of the core sample.
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Blue
Mud! One half of the core on the work table in the lab.
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This
was the fastest core sample taken yet--perfect mechanical operations
and a shallow summit at 1235 meters. (Shallow? That’s almost 4000
feet, but shallow compared to where we’ve been.) The gravity core
plunged deeply into the mud but again came back with a short sample.
It may have been short, at 24 inches, but it was BLUE MUD! There was
no sediment on the surface at this location on the seamount. Four
inches of green serpentine mud and the rest is layers in various shades
of blue serpentine ranging from a lovely pale blue to a deep blue
like the night sky. Blue mud, the consistency of clay--a pottery maker
would love this stuff. I wanted a sample for myself but you can’t
do mud pies around all these geologists and chemists. |
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Mariana Forearc was first dredged in 1981 so the presence of serpentine
mud has been known for over 20 years. It wasn’t until early 1990,
when drilling was done at Conical Seamount, that the seamounts were
discovered to be volcanic in nature. Patty
discovered the blue serpentine in 1997, from this very ship, at Pacman
Seamount. I wish I had been there. Patty still sparkles as she describes
the moment the core pipe was opened and the bright blue mud was first
seen. |
Geoff
is taking samples to study the chemistry of the core water.
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Jim
and Andrea. Andrea is taking
samples to study microbes.
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The
serpentine, as it first forms from periodotite deep beneath the seafloor,
is blue. It changes color to green as it seeps closer to the volcanic
summit and interacts with sea water. The exact chemical processes
involved here are not completely understood and are being studied
during this expedition. Patty has found blue mud at South Chamorro,
Blue Moon, Celestial, Big Blue, and Pacman Seamounts. |
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Back
into the water with Medea and the DSL-120 at 1300, results in a
perfect decent and a beautiful start to the 8 transects planned
over Big Blue Seamount.
Day
9: The DSL-120 survey of Big Blue Seamount continues all day today
and, probably, through the night. Medea is working beautifully as
the weight for the DSL fish. Akel tells us the data is magnificent
and will result in spectacular maps. Everything is going so well
that the plan has expanded to include a deep water transect starting
at the base of the seamount. We finished transect 8 just before
sunset. The ship is now towing the DSL-120 south. Eight miles from
the summit, at a depth of 3150 meters, we will start a single transect
from the deep water up the south flank and over the summit of Big
Blue.
In
the control van when Jason II is working, it’s exciting watching
the monitors—the sea floor, the navigation, and the placement and
retrieval of the scientific equipment and samples. In the control
van with the DSL-120 there is not the same thrill. During my last
watch, Tito, the pilot, explained
that watching the DSL-120 is as much fun as watching grass grow.
Tom, the navigator, said
it wasn’t that exciting, it was more like watching paint dry.
Science
Summary - Day 8 & 9, March 30 & 31
Science
Objectives, Days 8 and 9:
The
eighth and ninth days of the cruise, March 30 -31, will be spent
surveying Big Blue seamount. We will be finishing the transit to
Big Blue seamount where we will drop transponders and navigate in
the transponder net for our DSL-120 survey. A transect across the
summit with EM300 will give us bathymetry to help plan the DSL-120
survey. We want to do a gravity core at the summit then will deploy
DSL-120 and spend the rest of day eight and all of day nine finishing
the survey of Big Blue Seamount. The survey will include a transect
up the entire south flank of the seamount along a multi-channel
seismic line collected in 2002 on the R/V Ewing. We will retrace
the multi-channel seismic line to ground-truth features observed
in the seismic profile.
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