shape, elongated in the east-west direction
with an east-west-striking fissure swarm, as well as a radial dyke system, extending from
the small summit crater (Jónsson, 1988; Einarsson and Brandsdóttir, 2000). The southern
flank of the mountain has been eroded by the
outlet-glaciers and rivers which extend from
the ice cap. Reversely magnetized rock can be found in the gulleys formed, indicating
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf