"he sees a glacier in action from below"). Here he saw that the glacier has holes filled with water, these pockets can contain up to about twenty litres of water. The commentator puts forth the hypothesis that these pockets are generated by the pressure of the ice mass above and that these holes make the glacier less rigid and hence move faster.
The beautiful thing about glaciers is that they are rivers of ice, really behaving like a liquid. The bottom meter (or so) is even filled with sediments (sand, gravel, stones) like they are picked up by the flow and then whirled into the ice. (We even have a word for these processes: glaciofluvial.)
A typical glacier will move several meters (up to about 30 meters) a day, with the bottom parts moving slower due to the friction with the bed. However, the enormous pressure in the bottom parts of the glacier, make the ice more fluid than that on the top layers. During the flow the top layers of the glacier will often crack, because this part (the 'fracture zone') is so rigid.
Now, I was wondering. May it not be possible that the pockets of water in the lower parts of the glacier are a result of a solid phase water being forced into the liquid phase by the energy the glacier has to absorb on its way?
I tried to find an answer on this wonderfully informative site: Martin Chaplin's Water structure and science (here: phase diagrams). however, I could not find the answer there easily. Probably, because most of the information on the site is too specialised for me (or maybe even just too difficult and complicated).
By the way, it seems that the water in these pockets can't be colder than -20°C; looking at the phase diagram from professor Chaplin's site.
What a wonderful place we live in!