Islas Salomón · Estratovolcán
Tinakula
- Tipo
- Estratovolcán
- Altitud
- 796 m
- Última erupción
- 2024

- Tipo
- Estratovolcán
- País
- Islas Salomón
- Región
- Pacífico Suroccidental / Vanuatu Volcanic Arc
- Altitud
- 796 m
- Coordenadas
- -10.386, 165.804
- Última erupción
- 2024
- Contexto tectónico
- Zona de subducción / Espesor de corteza desconocido
- Forma volcánica
- Compuesto
- Roca principal
- Andesita / Andesita basáltica
Resumen geológico
The small 3.5-km-wide island of Tinakula is the exposed summit of a massive stratovolcano at the NW end of the Santa Cruz islands. It has a breached summit crater that extends from the summit to below sea level. Landslides enlarged this scarp in 1965, creating an embayment on the NW coast. The Mendana cone is located on the SE side. The dominantly andesitic volcano has frequently been observed in eruption since the era of Spanish exploration began in 1595. In about 1840 an explosive eruption apparently produced pyroclastic flows that swept all sides of the island, killing its inhabitants. Recorded eruptions have frequently originated from a cone constructed within the large breached crater. These have left the upper flanks and the steep apron of lava flows and volcaniclastic debris within the breach unvegetated.
Resumen de Wikipedia
Resumen en inglésTinakula is a conical stratovolcano which forms an island north of Nendo in Temotu Province, Solomon Islands. It lies at the north end of the Santa Cruz Islands. It is about 3.5 kilometres wide and rises 851 metres above sea level, rising three to four kilometres from the sea floor. The volcano was first recorded in eruption in 1595 when Spanish explorer Álvaro de Mendaña sailed past it during his second expedition across the Pacific Ocean. Tinakula has also been known in the past as Tamami or Volcano Island.
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Historial de erupciones
28 registradasGlosarioLínea de tiempo detallada
- 2018VEI 2Observado2018-12-08 – 2024-12-31Summit vent and NW flank
- 2017VEI 3Observado2017-10-21 – 2017-10-26Summit crater
- 2008VEI 1Observado2008-09-19 – 2008-11-29
- 2006VEI 2Observado2006-02-11 – 2007-11-09
- 2002VEI 1Observado2002-04-16 – fin desconocidoUpper NW flank
- 2002VEI 1Método no indicado2002-11-16 – fin desconocido
- 2000VEI 1Observado2000-02-29 – 2001-05-08
- 1999VEI 1Observado1999-05-16 – fin desconocido
- 1995VEI 1Observado1995-07-02 – fin desconocido
- 1989VEI 1Observado1989-08-16 – 1990-02-16
- 1984VEI 2Observado1984-06-03 – 1985-06-13Upper NW flank
- 1971VEI 2Observado1971-09-06 – 1971-12-11Upper and lower NW flanks
- 1965VEI 3Observado1965-11-23 – 1966-06-11Upper NW flank
- 1955VEI 2Método no indicado1955-08-16 – 1955-10-15
- 1951VEI 3Observado1951-10-23 – 1951-11-27
- 1932VEI 1Observado1932-05-11 – fin desconocido
- 1927VEI 2Observado1927-03-01 – 1927-03-04
- 1909VEI 2Observado1909-08-16 – fin desconocido
- 1897VEI 2Observado1897-03-26 – fin desconocido
- 1886VEI ?Observado1886-07-02 – fin desconocido
- 1871VEI 2Observado1871-09-16 – 1871-09-19
- 1869VEI 2Observado1869-03-16 – fin desconocido
- 1855VEI 2Observado1855-08-16 – 1857-08-16
- 1840VEI 3Observado1840-07-02 – fin desconocido
- 1797VEI 1Observado1797 – fin desconocido
- 1767VEI 2Observado1767-08-17 – fin desconocido
- 1595VEI 3Observado1595-09-07 – 1595-09-14
- 1050 a. C.VEI ?Estimación geológica1050 a. C. – fin desconocido
Volcanes cercanos
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.