BackgroundThe massive El Hierro shield volcano is truncated by a large NW-facing escarpment formed as a result of gravitational collapse of El Golfo volcano about 130,000 years ago. The steep-sided 1500-m-high scarp towers above a low lava platform bordering 12-km-wide El Golfo Bay, and three other large submarine landslide deposits occur to the SW and SE. Three prominent rifts oriented NW, NE, and south at 120 degree angles form prominent topographic ridges. The subaerial portion of the volcano consists of flat-lying Quaternary basaltic and trachybasaltic lava flows and tuffs capped by numerous young cinder cones and lava flows. Holocene cones and flows are found both on the outer flanks and in the El Golfo depression. El Hierro contains the greatest concentration of young vents in the Canary Islands. Uncertainty surrounds the report of an historical eruption in 1793 at Volcano of Lomo Negro. Source: Smithsonian GVP
El Hierro Photos
A storm arises on El Hierro, Canary islands. (Photo: Janka)
South rift zone landscape, El Hierro Island (Canary Islands) (Photo: Tom Pfeiffer)
Lava bomb at Playa de Verodal/El Hierro (Photo: Tobias Schorr)
Big surf at the west coast of El Hierro Island. The coast is formed by Holocene basalt lava flows forming a plateau that is exposed to the full force of the ocean waves. ...
El Hierro volcano tours:Europe's Volcanic Outpost (Walking and study tour to the Canary Islands: Lanzarote, La Palma, El Hierro and Tenerife)
See also: Sentinel hub | Landsat 8 | NASA FIRMS