Report on Hierro (Spain) — 15 February-21 February 2012
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 15 February-21 February 2012
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2012. Report on Hierro (Spain). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 15 February-21 February 2012. Smithsonian Institution and US Geological Survey.
27.73°N, 18.03°W; summit elev. 1500 m
All times are local (unless otherwise noted)
Instituto Geográfico Nacional (IGN) reported that during 15-16 February the amplitude of the tremor showed very low values, and after 17 February the tremor signal could not be clearly recognized in the seismic records. Very weak and intermittent discoloration was observed in the emission area. By the end of the reported period, there was no clear instrumental evidence of continuous eruptive activity.
One hundred and thirty-five seismic events were located, most of them in the central part of the island, with offshore events extending to the S. Depths of the hypocenters varied between 6 and 20 km and magnitudes between 0.2 and 2.5 (91 events with a magnitude equal or greater than 1). One event was felt by residents with a maximum intensity value of II (EMS-98). GPS data pointed to a slight uplift in some stations located at the N of the island.
Geologic Background. The triangular island of Hierro is the SW-most and least studied of the Canary Islands. The massive 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 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. Hierro contains the greatest concentration of young vents in the Canary Islands. Uncertainty surrounds the report of an historical eruption in 1793.