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Daily Updates: May 2000 |
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TODAY'S WEATHER
Cloudy
86°F (30°C)
Latitude: 11 deg 38N
Longitude: 101 deg 18W
Wind Direction: NE
Wind Speed: 13 Knots
Sea State: 2
Swell(s) Height: 3-5 Foot
Sea Temperature: 84.2°F (29°C)
Barometric Pressure: 1012 MB
Visibility: 10-25 Nautical Miles
Breakfast
Ham & Cheese Omelet
Poundcake
Pancakes & Sausage
Hash Browns & Oatmeal
Eggs to Order
Peaches & Yogurt
Lunch
Cheese Burgers
French Fries
Baked Beans
Pepper Pot Soup
Peanut Butter Crispy Bars
Dinner
BBQ Chicken
OBrien Potatoes
Mushroom & Onion Quiche
Fresh Baked French Bread
Sour Cream Chocolate Chip Cake
Homemade Cherry Nut Ice Cream
Click here to see a movie of a hydrothermal vent.
Farewell from Expedition #3!
May 8, 2000
By Dr. Dan Fornari
As RV Melville cuts through the low, broad Pacific
swells at 12.5 knots on a northwest course towards Manzanillo,
Mexico, the scientific and technical teams on board have nearly
finished packing. In fact, the computer I am using to write this
last daily journal will be boxed up and put in the shipping vans
tomorrow morning. Everyone on board is starting to relax after
6 weeks of nonstop activity. There is a lot of excitement and anticipation
of arriving in Manzanillo on Wednesday and, for the science team
and some of the crew, heading home before week’s end.
What have we accomplished during this cruise? It
has been spectacularly successful! We have mapped in detail and
sampled three previously unexplored areas of the mid-ocean ridge
crest where the Autonomous Hydrophone Array (AHA) had detected
seismic events over the past few years. When we get back to our
home institutions, we will begin many months, even years, of analyses
and interpretation of the sonar and photographic data, and the
rock samples. We will relate our sonar images of the seafloor to
the bathymetric maps to learn about the sizes and shapes of volcanoes
on the mid-ocean ridges. We will identify new lava flows from all
the images that we have collected to determine which volcanoes
erupted recently. We will test whether those recent eruptions are
related to the seismic events detected with the hydrophones by
determining the ages of the freshest lavas we have collected. Will
the age of the rocks match the timing of the earthquake activity?
Only time (and a lot of painstaking scientific work) will tell!
Mike Perfit and his students will analyze the volcanic
glass samples that we have collected to determine their chemical
compositions. From those data, they will be able to reconstruct
the history of the lavas -- how deep in the Earth they came from,
whether they pooled in a magma chamber before erupting on to the
seafloor, and how each lava flow is related to the others. Just
like a jigsaw puzzle, this information will be fitted together
with all the other data to learn about how the ocean floor is built
along the mid-ocean ridge over thousands of years, as well as in
episodic bursts that may last only days.
We also discovered new sites of hydrothermal activity
on the East Pacific Rise near 1° 40’N. What is the heat
source driving the circulation systems? Is it a new lava flow,
or a new fault that opened up a crack deeper into the Earth? Could
their development be related to the three-year old seismic event
detected by the hydrophones at that site? Can our data provide
new insights to answer these questions?
The Science Party of Expedition #3
For now, it is “farewell” from
all of us on board the RV Melville! We have enjoyed being able
to Dive and Discover with you on the East Pacific Rise and Galapagos
Rift during this expedition -- thank you for participating!
Next spring, we are going to the Indian Ocean to explore for hydrothermal
vents that have never been seen before! Will we be able to find
vents there? Will they be different from those we have found in
the Atlantic and Pacific Oceans? What will the animals that live
at vents in the Indian Ocean look like? There are different types
of animals on the different continents on land--is the same true
in the deep ocean? Will Indian Ocean vent animals be the same as
those around Atlantic Ocean or Pacific Ocean vents? Or, since the
Indian Ocean is between those two oceans, will they be a mixture,
or completely different? Can we learn something about how vent
animals spread from ocean to ocean, and vent to vent? Join us as
we use the remotely operated vehicle (ROV) Jason to get a close
look at the first hydrothermal vents ever seen at the mid-ocean
ridge in the Indian Ocean!
Personal Footnote –
I wish to thank my colleague Dr. Susan Humphris, my Co-Principal
Investigator on the Dive and Discover project, for the significant
help she has provided in the content, organization and writing
of the web site material for this expedition. In addition, Lori
Dolby and Danielle Fino at Woods Hole Oceanographic Institution
(WHOI) were Web Masters for the site, and their tireless efforts
back on shore to make the site superb are greatly appreciated.
Lonny Lippsett, Steve Lerner and Andy Maffei, all at WHOI, provided
additional editorial support and SeaNet support and I am very grateful
to them for their collaboration. Finally, I want to sincerely thank
all of my Co-Principal Investigators on Expedition #3, the wonderful
group of students, skilled technicians, and the officers and crew
of RV Melville, for contributing greatly to the success of the
science program and the Dive and Discover web site. None of this
work could have been done without them.
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