Satellite image of the 2025 Kaldalonsjökull. This is a composite image with some rough joins.......
As I pointed out in a previous post, this is a complex landscape of rocky knolls, platforms controlled by flat-lying basalts, wide gorges and narrow meltwater channels. Some of the undulating terrain still supports patches of dead ice -- elsewhere the ice has gone altogether, to be replaced nowadays just by a seasonal snowcover which changes from year to year in respose to precipitation totals and the directions of snowdrifting. There are traces of pitted moraine, fluted moraine and ridged moraine, probably related to recent glaciological conditions -- ie ice wastage within the last few decades.
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