Stunning curve with volcanic strata. In this volcanic landscape in Tenerife (Canary Islands), the white layer in the Curva de la Tarta (‘Cake Curve’) was formed by fragments of pumice and is very porous and light; the black and red layers were formed by basaltic cinder. In the area there is a gazebo with panoramic views of the sea of ??clouds that often cover the Orotava Valley, at the foot of Mount Teide.