Exploring
for New
Seafloor Eruptions
Expedition 3:
Mar 24-May 10, 2000
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Mail Buoy
April 9, 2000
Dear dive and discover:
I am interested in marine mammals. Can you tell me about anything
concerning marine mammals you have discovered on your voyages?
Thank You Joanna Grillo
Dear Joanna:
The Pacific Ocean is home to many different species of marine mammal,
including the largest animal in the world, the Blue Whale. Unfortunately,
we have not been lucky enough to see one of these rare creatures,
but we have seen groups, or pods, of pilot whales and porpoises.
These animals seem to enjoy being around the ship where they can
play in our bow wave and feed on the hundreds of fish which seem
to follow us wherever we go.
As we get closer to the Galapagos Islands, we can expect to see
the many sea lions which live on the islands. The islands are home
to other great marine animals, including Penguins and the famous
Marine Iguanas. The Iguanas are big lizards which dive underwater
to feed on the algae growing on the rocks.
Keep checking the website and when we see more marine mammals and
the animals of the Galapagos we’ll post it for everyone to
read, hopefully we’ll get some good pictures too.
Best Regards,
Ben Wigham
Dear Sir/Madam:
I would like to know the location of the following ocean trenches:
1. Kurile-Kamchatka trench
2. Mariana trench
Ina Pranoto
Secretariat of Convention on Biological Diversity
Dear Ina:
I hope this answers your questions. Thank you for viewing the website,
I hope you enjoy the rest of our voyage.
1. The Kurile-Kamchatka trench is located in the Western Pacific
Ocean. It runs northeast off the coast of Hokkaido, Japan, to the
Kamchatka Peninsula on the coast of eastern Russia. Here it joins
the Aleutian Trench which runs east across the northern Pacific
to Alaska. At its deepest point, the Kurile-Kamchatke trench is
approximately 9,750m deep.
2. The Marianas trench is also located in the Western Pacific,
it runs south from the Japanese coast, near Tokyo, towards the
Pacific island of Guam. It is famous for being the location of
the world’s greatest ocean depth. This point of the trench
is called Challenger Deep and is approximately 10,915m deep.
Best Regards,
Ben Wigham
I’m a mining engineer. Based on minerals present, what are
potential ore materials? And is the amount of minerals deposited
enough for future exploration and subsequent extraction? Or looking
at the larger picture, being the ocean as the next frontier, is
mining at that depth and condition possible?
Thanks and best regards,
Adrian CV Manlagñit, Philippines
Dear Mr. Manlagñit:
There are certainly mineral deposits on the seafloor, in fact some
of the world’s best copper ore deposits were formed at seafloor
hydrothermal settings. An example is the large copper ore deposit
in Cyprus. There are also other types of mineral deposits which
form in the deep ocean basins, like manganese nodules. At this
point, however, it appears that the economics of deep ocean mining
do not justify extensive efforts at exploiting seafloor mineral
deposits. There are also environmental concerns that must be taken
into consideration.
I hope this is information is helpful to you. Thanks for your participation
in Dive and Discover.
Best Regards,
Dan Fornari
Hello to all of you. I actually have 2 questions,
I hope you don’t
mind. You have analyzed previous data and are now gathering your
own data. Will you come back to this particular area on the ridge
to see how things have changed or to do further research? Also,
looking at past data and the present data, how far apart has the
crust spread at this ridge?
Cat Dayton
Reilly School
Hi Cat:
Thanks for your questions. We have collected data from two areas
of the East Pacific Rise so far on this cruise. One area, near
9-10°N latitude, we have studied extensively for the past decade
and we are comparing how the seafloor and hydrothermal vents look
each time we go there. The second area we have surveyed so far,
near 3°20’N, has never been visited before so what we
found during this cruise is the baseline, or the first data set
that will give us the ability to see how the ridge crest topography
changes over the coming decades and beyond. In the future, other
scientists will be able to use our data to make these types of
comparisons. The mid-ocean ridge in this area of the eastern Pacific
Ocean is spreading apart the Pacific and Cocos Plates at a rate
of about 11-13 centimeters per year; that is the full spreading
rate or how fast the separation between the two plates is occurring,
each side is moving at half that rate.
Hope these answers are helpful. Thanks for Diving and Discovering
with us.
Best Regards,
Dan Fornari
I was wondering how much does water temperature vary from surface
to ocean floor at active margins of the East-Pacific Rise, I know
temps. stay fairly constant at the tropics but It would seem logical
that the surface would be warm then as you increased in depth it
would grow considerably cooler, but closer to the spreading center
would the temperature increase due to the volcanic activity? And
I was also wondering if intense volcanic activity along the East
Pacific Rise could play a role in the El Nino’s in the that
region?
Thank You,
Terry Covey
Geology Undergrad. at Western Illinois University
Hi Terry:
Great question! As you can see from the sea surface temperatures
posted in the daily weather of Dive and Discover, the ocean water
temperature is quite warm, about 85°F. At the bottom, the water
is near freezing. But when there are volcanic eruptions on the
mid ocean ridge crest, the water near the seafloor gets a little
warmer, by usually less than a degree. However, it is significant
because of how constant in temperature bottom water is at the depth
of the ridge crest; which is around 2500 meters. Scientists have
used small, discrete increases in temperature associated with recent
seafloor eruptions and vigorous hydrothermal venting to actually
find new lava flows on the seafloor. As to whether intense hydrothermal
and volcanic activity could propagate upwards in the ocean and
influence El Ninos, I suspect that would be difficult, but there
have been times in the geologic past where seafloor volcanism has
been intense, and perhaps it could have then. It is an idea that
oceanographers have considered but do not think likely at this
point.
Thanks for your questions and keep Diving and Discovering with
us.
Best Regards,
Dan Fornari
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