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Global Volcanism Program | Image GVP-06142

Pico de Teide towers above the Llanos de Ucanca plain on the floor of Las Cañadas caldera.  The rocky spires in the foreground are eroded remains of intrusive phonolitic rocks of the Cañadas formation, predating formation of the caldera.  Youthful dark-colored lava flows blanket the SW (left) side of Teide.  The upper limit of the snowfield just below the summit of Teide marks the rim of the summit crater. Copyrighted photo by Katia and Maurice Krafft, 1977.

Pico de Teide towers above the Llanos de Ucanca plain on the floor of Las Cañadas caldera. The rocky spires in the foreground are eroded remains of intrusive phonolitic rocks of the Cañadas formation, predating formation of the caldera. Youthful dark-colored lava flows blanket the SW (left) side of Teide. The upper limit of the snowfield just below the summit of Teide marks the rim of the summit crater.

Copyrighted photo by Katia and Maurice Krafft, 1977.

Copyrighted image used with permission. All Rights Reserved. Contact photographer for any usage requests.


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