Volcanoes and Peaks
The Canary Islands are a volcanic archipelago shaped by millions of years of tectonic activity. This collection features prominent summits and volcanic structures across the islands, including the basaltic monoliths of La Gomera, the ancient Los Ajaches massif in Lanzarote, and the recent cinder cones of La Palma. These sites showcase diverse geological formations such as phonolitic necks, oxidized craters, and rugged ridges formed by cooling lava and extensive erosion.
Risco Grande
A prominent peak in the central highlands of Gran Canaria, located within the Nublo Rural Park.
Montaña de Aguas Sabinas
A summit in the northwest of Gran Canaria, situated near the Tamadaba Natural Park.
C Roque de Agando
Roque de Agando is a prominent rock formation on the island of La Gomera in the Canary Islands.
D Roque de Taborno
A distinctive basaltic neck in the Anaga Rural Park of Tenerife. This sharp-edged monolith is an erosional remnant of the island's ancient volcanic complex.
Montaña Colorada
A volcanic cone in northern Fuerteventura characterized by its deep red volcanic soil. It forms part of the Bayuyo alignment of volcanoes near Lajares.
F Montaña Negra
A black cinder cone in Tenerife located near the Chinyero volcano, surrounded by extensive fields of dark lapilli and basaltic lava flows.
Montaña Caldereta
A well-preserved volcanic crater in Lanzarote's Los Volcanes Natural Park, showcasing the island's stark, arid geological features.
Restinga
Volcanic landscape on the southern tip of El Hierro, notable for the 2011 submarine eruption that occurred just offshore from the coast.
Atalaya de Fémes
The highest peak in the Los Ajaches massif of Lanzarote. At 462 meters, it is part of the oldest geological formation on the island.
Teneguía
Teneguía is a monogenetic cinder cone – a volcanic vent which has been active once and has had further seismic activity.
Teneguía
Teneguía is a monogenetic cinder cone – a volcanic vent which has been active once and has had further seismic activity.
Teneguía
Teneguía is a monogenetic cinder cone – a volcanic vent which has been active once and has had further seismic activity.
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