17 November, 1998
Today our main goal was to do some ice coring at Lake Vida, another lake in the Dry Valleys. My team is trying to get as many samples as possible so that they have a lot to work with when they're doing experiments. They are trying to compare the similarities and differences among the various lakes. What makes them different? What makes them the same? Are the same organisms found at each lake? The locations of the lakes are very different, obviously, but the surfaces are very different (some are very rough, some are relatively smooth). Some lakes have ice full of bubbles; some lakes have the clear, dark blue ice that you can see great distances through. It's interesting to see how different each lake's ecosystem is.
I woke up at 7:30 am and checked my e-mail before breakfast. I packed a day pack for the trip to Lake Vida (water bottle, pee bottle...that's what they're called!, snacks, and sample bottles...in case we find any sediments we want to sample). At 10:30 the Kiwi helicopter arrived and dropped off another visitor, a Boy Scout named Ben Hasse. He was selected from many Boy Scouts for the honor of traveling to Antarctica to visit all of the stations and scientists down here. He just returned from a trip to the Pole, and now he'll be with my team until Saturday when everyone is returning to McMurdo for the weekend.
Mark and Chris are joining us for the day to help us collect samples. So, John, Chris, Nina, Mark, and I were on our way to Lake Vida for the day. We arrived around 11:00 am and immediately began coring. The weather was extremely nice...very warm and sunny. We cored for about an hour and realized that we really weren't getting good cores...the ice was crumbling into smaller puck sizes, rather than long sections of cylindrical ice. To core ice, we use a long cylindrical metal tube with spiral cuts on the outside and a drill bit on the bottom (to cut into the ice). On top of the cylinder, we place a power head (basically an engine...you start it like you would a generator or a lawn mower...by pulling the cord). The power head causes the cylinder to turn, and hopefully, by pushing down on the cylinder barrel, we can take cores of ice out of the lake. [Today it wasn't working very well.] The ice core samples are then gently tapped into a relatively clean trough so that they can be bagged, labeled, and placed into a cooler for transportation back to the Crary Lab freezers at McMurdo.
We ate our boxed lunches that Chris had brought from the Galley at McMurdo. We decided to try a couple more cores to see if it mattered where we were coring. This took us until about 3:30 pm. As we rotated jobs, we had to keep warm, so we played "Keep Away" with some duct tape. That ended when Mark got hurt...he pulled a muscle. Actually, after that it really warmed up. The wind stopped and that's when my temperature gauge on my jacket fluctuated between 40 and 50 degrees F! We took layers off and decided to go for a walk to the stream bed (which was about a 45-minute walk from where we cored) to gather algae samples. We found huge algal mats lying in the snow off-shore. Remember I said that the algae is easier to find in meltwater areas? That's where we found them...in the dirty snow that was half-melted. At 5:00 pm the helicopter picked us up to take us back to Lake Bonney. On the way, we stopped at Marble Point to refuel (just a home-away-from-home for fueling). Ed made us halibut steaks, boiled cabbage, and broccoli/cheese rice...very good! Being out all day made me tired, so I went to bed around 10:30, a little earlier than the last few nights.
Contact the TEA in the field at .
If you cannot connect through your browser, copy the TEA's e-mail address in the "To:" line of your favorite e-mail package.