They have really good meals over there so it was a good reprieve. I can't remember everything we ate except I remember that they had real ice cream! That was good.
Afterward, we hung out in their bar (I had a Sprite. They have American night once a week where all the Americans can come, but it wasn't last night. I've heard it's a lot rowdier when all the Americans swarm the place) and I went on a tour of the base. Everything is connected together which is very useful in the Antarctic winters. It's definitely not as big and sprawling as Mactown.
Scott Base, Antarctica |
Miers is a pretty small valley with two glaciers, a stream, and a lake.
Our job was to set up a total of 9 sites (3 at each elevation) going down the mountainside. We also needed to collect 3 samples at each of the sites. Since it's so cold in the Dry Valleys, the soil forms these interesting shapes called polygons. We needed to find polygons that were big enough to fit our plots so it took a little while to find the right location. While Martijn, Zach, and I did that, Byron set up a meteorological station. The station collects soil temperature and moisture year-round.
The technical name for polygons is thermal contraction crack polygons. They have been found on Mars and in the Arctic as well. They form in Antarctica because the soil freezes then thaws repeatedly. When we walk around in the Dry Valleys, we try to only walk in the cracks so it can make a relatively short journey take a lot longer.
After we were done sampling, we only had a few minutes left before the helicopter came to pick us up again. I took a picture of a ventifact, which is a rock that has been shaped and hollowed out by wind-blown sand. I also got a picture next to the stream running through the valley.
Overall, it was a great final day of field work in the Dry Valleys of Antarctica!
Polygons on the side of Miers Valley |
A ventifact a few hundred yards from the stream in Miers Valley |
Standing next to the stream with both glaciers in the background |
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