In the previous post, the glacier can be seen struggling to overcome it´s own end morain (which is by the way not formed by the ice pushing the underlying material, but rather by surface waters flowing off the end of the glacier and depositing sediments in front of it).
At that time, around 1900, the glacier is at absolute maximum for the entire Holocene (the last 8000 years), but today it is seriously reduced and cannot be seen at all from where the original picture is taken.
I found a fairly good picture on the net, taken by a David Elliot (sorry for stealing your picture, David!) where he has gone behind the end moraine (first picture). This particular glacier is rather fast moving (which can be seen by the cracking) and has a tendency to advance and retreat regularly, but since I started going there in the 1990s, the glacial tongue proper has thinned by several tens of meters.