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Mirador de La Tarta del Teide

Mirador de La Tarta del Teide

Updated 2 August 2026
La Orotava
Pyroclastic rock formation with colored layersWhite layer of porous and light pumiceBlack layers of basaltic scoria from eruptions

The Mirador de La Tarta is located next to the TF-24 road, on the section that ascends from La Laguna towards El Portillo and the Teide National Park. In front of it rises La Tarta del Teide, a pyroclastic rock formation that constitutes an ancient lava river resulting from successive volcanic eruptions. Its striking colored stripes give it its name: the white layer is made up of pumice stone fragments, the black layers of basaltic scoria from low-emission eruptions, and the reddish ones from the same scoria oxidized by contact with groundwater.

Centuries or millennia could have passed between the formation of one layer and another, making the slope one of the most recognizable geological stops on the ascent to Teide.

Essential information

Accessibility

Access is via the TF-24 road at km 31.8-31.9; it is advisable to stop at nearby pullouts to observe the formation up close.

Risk Level

It is a roadside stop on a mountain road: park only in designated pullouts and exercise extreme caution with traffic when stopping.

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