Landslides have been a key process in the evolution of the western Canary Islands. The
younger and more volcanically active Canary Islands, El Hierro, La Palma and Tenerife …

Understanding the structure and development of calderas is crucial for predicting their
behaviour during periods of unrest and to plan geothermal and ore exploitation. Geological …

The growth and decay of oceanic hotspot volcanoes are intrinsically related to a competition
between volcanic construction and erosive destruction, and coastlines are at the forefront of …

Because of their social, economic and political contexts, and their intrinsic multi-hazard
nature, volcanic islands are one of the most vulnerable environments, where natural …

Abstract The Teide and Pico Viejo stratocones and the Northwest and Northeast Rifts are
products of the latest eruptive phase of the island of Tenerife, initiated with the lateral …

The morphology and structure of the submarine flanks of the Canary Islands were mapped
using the GLORIA long‐range side‐scan sonar system, bathymetric multibeam systems, and …

The petrology, geochemistry and petrogenesis of the active Teide–Pico Viejo volcanic
complex provide information about the evolution and internal structure of the Tenerife central …

Volcano slope instability manifests in many forms, ranging from steady state to punctuated
movement, or shallow erosion to deep-seated spreading. The interplay of gravity, magmatic …

The structure and volcanic stratigraphy of the Pico Teide–Pico Viejo (PT–PV) formation,
deriving from the basanite–phonolite stratovolcanoes PT and PV, and numerous flank vent …

The Las Cañadas caldera is one of the most important geological structures of Tenerife.
Stratigraphic, structural, volcanological, petrological, geochronological, and geophysical …