The biggest task this week has been preparing samples to be shipped north. I've got all kinds of samples that all have different processing and transportation requirements. It's kind of like trying to figure out how to load a grocery bag. You want your ice cream to stay frozen, your apples not to get bruised, and your eggs not to crack. Only here, I need my ice cores (from Garwood) to stay frozen, my soils (from Taylor) not to grow mold, and my rocks (from everywhere) not to get chipped. Fortunately, the cargo vessel that will be docking in McMurdo next month has freezers, coolers, and giant storage containers aboard that should get my samples home safe and sound.
Since Antarctica is in the southern hemisphere, and Portland is in the northern hemisphere, the ship has to cross the equator to get my samples home. It's pretty impressive to think that the ship can keep ice cores at -20*C (-4*F), even when it's 90*F outside. Since my soils don't need to be in a freezer the whole way back, they need to be dried so that they don't grow mold in the heat (the same way foods like potato chips or raisins are dried to keep them from getting moldy).
I'd say it has been a great season. We've learned a lot about how the "invisible streams" in Taylor Valley (the water tracks) come out of their winter freeze. In Garwood, we've begun to explore a frozen world that existed almost 10,000 years ago. It's been an adventure at times:
|Sampling algal mats at the top of the Garwood Valley "ice cliff." It might not seem like much of an adventure, but to get there I had to cut toe holds in the ice...|
Stay tuned to this blog during the "off season" for updates on what we've found in the Dry Valleys, news about publications, and more stereo pictures!