Last night I got the opportunity to go on a walking tour of the pressure ridges. The pressure ridges are located near the New Zealand Antarctic base (Scott Base). They are the result of the collision of the annual sea ice and the Ross Ice Shelf. The sea ice melts (or at least thins considerably) during the summer months. When this happens, it weakens and is forced into pressure waves of ice as the ice shelf pushes against it. These waves eventually crack, and the pressure ridges are formed. They create large chunks of ice that stick up in all directions, creating an other worldly landscape. At the base of the ridges, the cracks can actually extend to the water below, creating holes for penguins and seals to come up through. Unfortunately, I saw neither on my trip, only footprints. It was definitely a very cool trip, and I will add it to the list of things that I have done down here, that I never thought I would ever get a chance to do in my life. Below are some pictures.
On the work side of things, there is a slight chance that we might launch the ULDB test balloon tomorrow evening. It looks like after tomorrow we will have an extended period of not so good weather, so everyone is working very hard to get the balloon and the payload ready in the hopes that we might be able to launch before the bad weather gets here. Everyone keep your fingers crossed.
Penguin tracks through the snow - you can see that it was sliding on it stomach and pushing with its back feet.
Me standing between 2 ridges with Mt Erebus in the background
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Pressure ridge, with Mt Erebus (background right) and Castle Rock (background left)
I thought this one looked like a shark