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. 2009 Nov 2;106(47):19770–19775. doi: 10.1073/pnas.0906029106

Fig. 3.

Fig. 3.

Photographs of two sections from the Kilimanjaro NIF core 3. (A) Appearance of the top 0.65 m that contained elongated bubbles, channels, and voids characteristic of melting and refreezing. (B) The remainder of the 49-m core to bedrock appears as glacial “bubbly” ice shown here, confirming the absence of features associated with melting and refreezing.