Saltar al contenido principal
← Volver al mapa
⇄ Comparar

Monte Paektu

Changbaishan

Estratovolcán · China-North Korea · 2744 m

Lake Tianchi occupies the 5-km-wide, 850-m-deep summit caldera of Changbaishan, which straddles the China/Korea border. The volcano is also known as Baitoushan and by the Korean names of Baegdu or P'aektu-san. This view looks from the northern rim on the Chinese side towards the SE caldera wall on the Korean side. One of the world's largest known Holocene explosive eruptions took place from Changbaishan about 1000 CE, depositing tephra as far away as northern Japan.
Lake Tianchi occupies the 5-km-wide, 850-m-deep summit caldera of Changbaishan, which straddles the China/Korea border. The volcano is also known as Baitoushan and by the Korean names of Baegdu or P'aektu-san. This view looks from the northern rim on the Chinese side towards the SE caldera wall on the Korean side. One of the world's largest known Holocene explosive eruptions took place from Changbaishan about 1000 CE, depositing tephra as far away as northern Japan. · Foto: Photo by Xiang Liu, 1983 (Changchun University). · Wikimedia Commons
Tipo
Estratovolcán
País
China-North Korea
Región
Eastern Asia Volcanic Regions / Central East Asia Volcanic Province
Altitud
2744 m
Coordenadas
41.980, 128.080
Última erupción
1903
Contexto tectónico
Intraplate / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Trachyte / Trachydacite
Resumen geológico

Massive Changbaishan stratovolcano (also known as Baitoushan and by the Korean names of Baegdu, Paektu, or P'aektu-san), is located along the China/Korea border. A 5-km-wide, 850-m-deep summit caldera is filled by Lake Tianchi (Sky Lake). The 60-km-diameter dominantly trachytic and rhyolitic volcano was constructed over the Changbaishan (Laoheidingzi) shield volcano. Satellitic cinder cones are aligned along a NNE trend. One of the largest known Holocene explosive eruptions took place here about 946 CE, depositing tephra as far away as northern Japan and forming in part the present caldera; Yang et al. (2021) estimated the total erupted volume to be 40-98 km3. Minor eruptions have been recorded since the 15th century.

Resumen de Wikipedia

Las montañas Changbai o Changbaishan ; ; en chino tradicional, 長白山地; en chino simplificado, 长白山地; pinyin, Chángbái Shāndì; Wade-Giles, Ch’ang-pai Shan-ti, también llamadas montañas Ohnan o cordillera de Changbai, de Šanggiyan o de Jangbaek, es una larga cordillera de Asia oriental que funciona como barrera natural entre las fronteras de la República Popular China, Corea del Norte y un pequeño tramo en Rusia. La mayoría de los picos tienen más de 2000 metros de altura, siendo el punto más elevado el monte Paektu.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
2155 BCE~1962 BCE · 1 erupciones · VEI máx. 41189 BCE~996 BCE · 1 erupciones · VEI máx. ?223 BCE~29 BCE · 1 erupciones · VEI máx. 4937~1130 · 1 erupciones · VEI máx. 61323~1517 · 1 erupciones · VEI máx. ?1517~1710 · 3 erupciones · VEI máx. ?1710~1903 · 2 erupciones · VEI máx. 22155 BCE1189 BCE223 BCE7441710

Línea de tiempo detallada

  1. 1903VEI ?Observado
    1903-04-15 – En curso
    Liuhaojie tuff ring?
  2. 1898VEI 2Observado
    1898 – En curso
  3. 1702VEI ?Observado
    1702-06-09 – En curso
  4. 1668VEI ?Observado
    1668-06 – En curso
  5. 1597VEI ?Estimación geológica
    1597-10-06 – En curso
  6. 1413VEI ?Estimación geológica
    1413 – En curso
  7. 946VEI 6Estimación geológica
    946-11-15 – En curso
    Millennium Eruption
  8. 180 a. C. (±80 años)VEI 4Estimación geológica
    BCE 180 – En curso
  9. 1000 a. C.VEI ?Estimación geológica
    BCE 1000 – En curso
  10. 2155 a. C. (±90 años)VEI 4Estimación geológica
    BCE 2155 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.