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3 March, 2000
Why No Seals, Whales or Penguins?
74 00 s 112 05 w
-11 C (12 F), wind 18 knots (21 mph) southwest
Barometer 988.9 mb, rising
Depth 726 m (2381 ft)
Clear, cold dawn. Crescent moon and a planet visible in the NW
North of Moore Dome, near Dotson ice shelf, Walgreen Coast
Some people have written me with comments on my journal entries,
and I thank all who have done so, especially those of you who have offered
suggestions. Please keep doing so! I have had two requests more than once,
so I thought I’d make some excuses… I mean offer explanations.
Why don’t I have more pictures of animals, especially seals or
whales? That’s an easy one to answer. Although I’ve seen a number of seals
and penguins (and one whale), I haven’t gotten close enough to any of them
to take a good picture. According to the “seal people” seals tend to rest
on the ice in the afternoon more than any other time. On an average day
I’ll see four or five. Mostly I see Weddell and Crabeater seals, but I have
also seen Leopard seals. I don’t actively watch for them like the “seal
people,” because I’m usually busy with other projects. So there must be
many I miss. They are fun to watch with binoculars, but if I tried to take
a picture, all you’d see is a little black smudge or two. It’s the same
with penguins. Although I see more penguins than seals, so far they have
been too far away to get good pictures. As soon as I can get a nice picture
or two, I’ll send them along. Emperor penguins look terribly dignified
standing up. When they want to move fast they get down on their bellies and
paddle along with their wings and feet. They glide so smoothly you would
almost think they were boats in calm water, rowing along.
The other comment, which came from several different people, is
that they would like to hear more about the day to day life on the ship,
about what living on a research vessel is like. That’s one I can fix more
easily. From time to time I’ll tell you about the more ordinary happenings
here.
My daily routine begins about 11 PM when I wake up to go on watch.
I go down to the galley and get something to eat and a cup of coffee. Since
people are working twenty-four hours a day, they have a meal from
11:30-12:30 called “midrats.” Don’t ask me where that word came from. From
midnight to three I usually do the geophysical watch that I was telling you
about. Then I do ping editing, write my journal, work on drying samples for
carbon dating, or go to the gym and get some exercise. I call that “wheel”
after the little exercise wheel my daughter’s gerbil has. There is a
stationary bicycle, a treadmill, a stair climbing machine and a rowing
machine. I used to use the bicycle all the time, but unfortunately it’s
broken now, so I use one of the others. I had trouble getting used to
running on a treadmill with the boat rolling and pitching in ice.
I try to watch the sunrise, if it’s not snowing or foggy. The sun
rises at about 2:30 and sets about 10:00 at night. It takes a long time to
rise or set, because its path is at such a shallow angle to the horizon.
When the sun rises, you see a tiny bit, called the upper limb, first. In
Maine, where I live, the sun takes only a minute or two to get completely
above the horizon. Here at 74 degrees south, I can go down to the galley,
get another cup of coffee, and come back on deck, and it seems like the
same tiny bit of sun is still there.
After breakfast I continue on watch, either using the radar to map
coastline, or go back on geophysical watch. I’m off watch at noon, but
after lunch I seem to just keep on doing the same things. Of course
everything else comes to a stop when there is a core to be taken. Sometimes
I help other groups like the ice people. I also spend a lot of time asking
questions and listening. I try to do this only when people seem interested
in talking! There are many fascinating people on board the Nathaniel B.
Palmer, crew and scientists, and they seem to have lots to tell.
I try also to play my fiddle at least twenty minutes a day. Some days I
play half an hour or more, and some days not at all. If we are coring in
deep water, it takes the corer about twenty minutes to go down to the
bottom and twenty to come back up. I usually wait in the same room where
Tom Kellogg is shown in the picture. I bring my fiddle and practice while
I’m waiting, if there is nothing else to do. There is enough noise from
machinery that it doesn’t bother people. I’m working on learning a tune
called Bay of Fundy (which also happens to be another glacial trough).
Once in a while we have emergency drill. No matter what you are doing, when
the brass alarm bells ring you have to grab warm clothes, boots, a survival
suit and a life preserver, and head for your assigned station. It doesn’t
matter if you’re sleeping, eating, in the shower, or on watch, you just
stop what you are doing and go. (Of course you put on some clothes first if
you are in the shower!) The halls are crowded with rushing people. When you
get to your alarm station, a crewmember takes roll call to make sure
everybody is there.
About four in the afternoon I begin to get really drowsy, so I climb in my
bunk and read for a little while. The ship rocks me and the engines hum me
to sleep, but not before I set my alarm for eleven o’clock. Life goes on
day after day like this, and weekends are pretty much the same as weekdays.
As a matter of fact, I often lose track of what day it is, and have to
check a calendar. Whatever day it is, I spend as much time as I can looking
outside. I want to store as much as I can for the future.
We have rounded Cape Herlacher and have been taking cores and CTD stations
along the front of the Dotson Ice Shelf. The Kohler Glacier feeds the
Dotson Ice Shelf. Cape Herlacher is on the northern tip of the Martin
Peninsula, which has the Murray and Slichter forelands. Nearby are Mt.
Murphy and the Thwaites glacier. At the eastern end of the Dotson Ice Shelf
is Bear Peninsula, with Moore Dome on one north facing tip. Of course
there are no bears in Antarctica, polar or otherwise. All these areas are
part of the Walgreen Coast.
Why did I list all those names? I was wondering how Bear Peninsula got its
name, since there are no bears around (the Arctic has polar bears, the
Antarctic has penguins.) Then I started wondering about all the other
names, so I looked them up. Here is what I found out.
Bear Peninsula is named after the USS Bear, a US Antarctic survey ship. The
ship was launched in 1874 in Scotland, and christened the Bear of Oakland.
It sank in 1963 after a long history of exploration. In the thirties and
forties, survey airplanes could be launched and retrieved from the Bear,
and these planes were first to explore this coast.
Carl J. Herlacher was a cartographer (mapmaker) for the US Navy in the
1930s. Walter J. Kohler, was an industrialist and governor of Wisconsin,
who helped buy the plane (launched from the USS Bear) from which the Kohler
glacier was first sighted. William Dotson was in charge of the Navy’s Ice
Reconnaissance Office, and was killed in a 1964 Alaska plane crash, while
on an ice watching mission. Lawrence Martin was an American geographer and
authority on Antarctic exploration for the Library of Congress. Grover
Murray was a geologist and member of the National Science Foundation’s
Board of Directors. Louis B. Slichter is a professor at UCLA, and has
trained many polar geophysicists. Capt. Robert Moore commanded the US
Coast Guard Cutter Burton Island, which explored this area in 1974-1975.
Robert Cushman Murphy was an authority on polar birds. He served on a
whaler in 1912-1913, observing birds and drawing charts in addition to his
normal duties. Fredrik Thwaites was a glacial geologist at the University
of Wisconsin. Last but not least, Walgreen Coast was named after Charles R.
Walgreen, president of Walgreen Drug Co. of Chicago. Walgreen was a
financial backer of Richard Byrd.
I searched through the book for places named after women. There are some
named for wives, daughters, queens or financial donors, but that was all I
could find. Can any body help me? Are there places named after prominent
women scientists or geographers? Girls, you may have missed out on the
first Antarctic explorations, but there’s still plenty of work to be done
here (and there are women on the Nathaniel B. Palmer doing it right
now.) How about the Moon and Mars? Things are changing!
The Transantarctic Mountains as seen from the Ross Sea. The famous dry valleys are up in those hills.
This is what you get when a Kasten core works well. One side of the square box is removable to get at the sediment. Dr. Tom Kellogg (shown scraping top of core) thinks that most of this core was deposited when the area was under a floating ice shelf, because it is very fine grained and has very few diatoms in it. He is scraping the top of the core so he can get a better idea of the color bands visible. The pink square at the top holds in the surface layers so they won't slump out.
The mate made a little snow couple to sit out on the bow. They don't seem at all bothered by the cold and the wind!
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