The Murray snowfield proved to be a long imperceptibly uphill slog in slightly soft snow, but no crevasse problems.
This is followed to a large crevasse in the upper face, which gives access to a small snowfield.
The other and larger tableland, which constitutes the substantial part of Iceland, reaches its culminating point in the south-east, in the gigantic snowfield of Vatnajokull, which covers 3300 sq.
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