Description :
Thick deposits of ice-contact sediments occur in a large valley north of Curtis Lake within a north-trending subglacial meltwater corridor - prominent esker ridges, apron pads and crevasse-fill ridges are found in association with subaqueous outwash fan deposits and glaciolacustrine sediments deposited in a proglacial lake trapped by the topographic drainage divide
Photographe :
McMartin, I
Collection :
Ressources naturelles Canada
Haute-résolution :
252.63 MB
3264x2448 pixels
180 ppi (jpeg)
Géographie :
2468; Curtis Lake; Nunavut