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 …

This paper reviews the evidence for onshore sedimentary imprints of tsunami inundation
known from the geological record of the Atlantic basin. The central aim of the paper is to offer …

The 2021 La Palma eruption provided an unpreceded opportunity to test the relationship
between earthquake hypocenters and the location of magma reservoirs. We performed …

Abstract Aim The General Dynamic Model (GDM) links island biogeographical processes to
island geological history. A key premise of the GDM implies that environmental factors …

The 1971 Teneguía eruption is the most recent volcanic event of the Cumbre Vieja rift zone
on La Palma. The eruption produced basanite lavas that host xenoliths, which we …

The formation and growth mechanisms of Mid-Ocean Ridges (MOR) are relatively well
known, whereas those of back-arc spreading ridges are comparatively less known because …

Marine conglomerates at high elevation on the flanks of ocean islands are usually
interpreted as evidence of mega-tsunamis generated by volcano flank collapses, although …

Some tsunami deposits have been previously identified 41–188 m asl in the Agaete Valley
on the northwest coast of the island of Gran Canaria, in the Canary Islands. In this paper, the …

Mass-wasting of ocean island volcanoes is a well-documented phenomenon. Massive flank
collapses may imply tens to hundreds of km3 and generate mega-tsunamis. However, the …

Sector collapses affect volcanic edifices across all tectonic settings and involve a rapid
redistribution of mass, comparable in scale to the largest magmatic eruptions. The eruptive …