Sampling map

miércoles, 30 de marzo de 2016

Debris bands

B1 - Debris band
B2 - Debris band



B3 - Debris band
Close-up of the debris band B3. Note the difference between the high debris content of the basal ice compared with the debris poor glacier ice, derived from the meteoric deposition  and compacting (firnification)

B4 & D3 - Debris band going disrupting some dispersed ice cryofactes section.

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