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Bárcena volcanoCinder cones 332 m / 1,089 ft
Mexican Islands (Mexico), 19.3°N / -110.82°W Current status: dormant (1 out of 5) [hide map] [enlarge map]
Typical eruption style: Explosive.
Bárcena volcano eruptions: 1952-1953  Last earthquakes nearby:
The volcano formed by eruptions during 1952-53 and consists in a 700 m wide and 330 m high tuff cone with a circular crater and a spectacular lava delta on the east side formed by a trachytic lava flow that breached the crater and entered the sea. The eruption was the first historic eruption witnessed in the eastern Pacific Ocean. Background:San Benedicto island is a 4.5 km long NE-SW elongated island composed of several volcanic vents that have migrated SW over time. Pleistocene trachytic lava domes form the northern part, and historical Bárcena volcano and Montículo Cinerítico, a smaller tephra cone preceding Bárcena and largely covered by it, form the southern tip of the island.Montículo Cinerítico may also have been constructed during the past few hundred years and formed the high point of the island prior to the formation of Bárcena. The formation of Bárcena began in August 1952 and was accompanied by strong explosive eruptions and pyroclastic flows including radial base surges. The eruption concluded the following year with the emplacement of two small lava domes in the crater and extrusion of a prominent coastal lava delta at the SE base of the cone. --- Source: GVP, Smithsonian Institution 1952-53 eruption
Barcena volcano was born during 's only historic eruption which began on 1 August 1952, from the El Boquerón vent. The eruption began with powerful vulcanian explosions creating base surges, which were witnessed from a nearby fishing boat. Large amounts of ash and pumice quickly built a new cinder cone built at the southern end of the island. In the later stage of the eruption, a viscous lava dome and lava flow emerged from the crater in December and flew to the east and created a spectacular, perfectly half-circular lava delta, known as the "Delta Lavico". ...more |
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