Volcán Bárcena
Barcena
Cono piroclastico · Mexico · 332 m

- Tipo
- Cono piroclastico
- Paese
- Mexico
- Regione
- Eastern Pacific Volcanic Regions / Mathematicians Ridge Volcanic Province
- Altitudine
- 332 m
- Coordinate
- 19.300, -110.820
- Ultima eruzione
- 1953
- Contesto tettonico
- Rift zone / Oceanic crust (< 15 km)
- Forma vulcanica
- Minor
- Roccia principale
- Trachyte / Trachydacite
Sintesi geologica
Volcán Bárcena, formed by eruptions during 1952-53, is the most prominent feature of the 4.5-km-long Isla San Benedicto, the NE-most of the Revillagigedo Islands, 350 km S of the tip of Baja California. Pleistocene trachytic lava domes form the north end of the island, with Bárcena and Montículo Cinerítico at the southern end. Montículo Cinerítico is a smaller tephra cone that preceded and was largely overtopped by Bárcena, and may also have been constructed during the past few hundred years. Growth of the 300-m-high Bárcena tephra cone beginning in August 1952 was accompanied by strong explosive eruptions and pyroclastic flows. The eruption concluded the following year with the emplacement of two small lava domes in the crater and extrusion of a coastal lava delta at the SE base of the cone.
Sintesi da Wikipedia
Riassunto in ingleseThe Bárcena volcano is an active but not currently erupting cinder cone type volcano that encompasses the southern end of the San Benedicto Island, Mexico. It is grouped with a chain of volcanic islands known as the Revillagigedo Islands. These islands are situated in close proximity to each other, and can be found in the Pacific Ocean. They are also considered to be part of the Trans-Mexican Volcanic Belt. Volcán Bárcena is positioned 220 miles off the south-eastern coast of the Baja California peninsula. The closest city to Barcena is Cabo San Lucas, Mexico.
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Storia delle eruzioni
Cronologia dettagliata
- 1952VEI 3Osservata1952-08-01 – 1953-02-24South end of Isla San Benedicto
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.