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Lassen Volcanic Center

Estratovolcán · United States · 3187 m

Lassen Peak, rising above Manzanita Lake on the NW, is the focal point of the Lassen volcanic center, a concentration of volcanic features covering much of Lassen National Park.  The massive lava dome forming Lassen Peak was constructed about 25,000 years ago and was the site of California's most recent eruption during 1914-1917.  Chaos Crags, a lava dome complex on the north flank, and the aptly named Cinder Cone to the NE, have also erupted within the past 1200 years.
Lassen Peak, rising above Manzanita Lake on the NW, is the focal point of the Lassen volcanic center, a concentration of volcanic features covering much of Lassen National Park. The massive lava dome forming Lassen Peak was constructed about 25,000 years ago and was the site of California's most recent eruption during 1914-1917. Chaos Crags, a lava dome complex on the north flank, and the aptly named Cinder Cone to the NE, have also erupted within the past 1200 years. · Foto: Photo by Dave Wieprecht, 1995 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Estratovolcán
País
United States
Región
North America Volcanic Regions / High Cascades Volcanic Arc
Altitud
3187 m
Coordenadas
40.492, -121.508
Última erupción
1917
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Lassen Volcanic Center consists of the andesitic Brokeoff stratovolcano SW of Lassen Peak, a dacitic lava dome field, peripheral small andesitic shield volcanoes, and large lava flows, primarily on the Central Plateau NE of Lassen Peak. A series of eruptions from Lassen Peak from 1914 to 1917 is the most recent eruptive activity in the southern Cascade Range. Activity spanning about 825,000 years began with eruptions of the Rockland caldera complex and was followed beginning about 590,000 years ago by construction of Brokeoff. Beginning about 310,000 years ago activity shifted to the N flank of Brokeoff, where episodic, more silicic eruptions produced the Lassen dome field, a group of 30 dacitic lava domes including Bumpass Mountain, Mount Helen, Ski Heil Peak, and Reading Peak. At least 12 eruptive episodes took place during the past 100,000 years, with Lassen Peak being constructed about 27,000 years ago. The Chaos Crags dome complex, ~3 km NNW of Lassen Peak, was constructed about 1,100-1,000 years ago. The Cinder Cone complex 17 km NE of Lassen Peak was erupted in a single episode several hundred years ago and is considered part of the volcanic center (Clynne et al., 2000). The 1914-1917 eruptions of Lassen Peak began with phreatic eruptions and included emplacement of a small summit lava dome, subplinian explosions, mudflows, and pyroclastic flows.

Resumen de Wikipedia

Resumen en inglés

Mount Tehama is an eroded extinct andesitic stratovolcano in the Cascade Volcanic Arc and the Cascade Range in Northern California. Part of the Lassen volcanic area, its tallest remnant, Brokeoff Mountain, is itself the second highest peak in Lassen Volcanic National Park and connects to the park's highest point, Lassen Peak. Located on the border of Tehama County and Shasta County, Brokeoff's peak is the highest point in the former. The hikers that summit this mountain each year are treated to "exceptional" views of Lassen Peak, the Central Valley of California, and many of the park's other features. On clear days, Mount Shasta can also be seen in the distance.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
800~911 · 2 erupciones · VEI máx. ?911~1023 · 1 erupciones · VEI máx. ?1580~1691 · 2 erupciones · VEI máx. 31803~1914 · 1 erupciones · VEI máx. 38001023135715801803

Línea de tiempo detallada

  1. 1914VEI 3Observado
    1914-05-30 – 1917-06-29
    Lassen Peak
  2. 1666VEI 3Estimación geológica
    1666 – En curso
    Cinder Cone
  3. 1650VEI ?Estimación geológica
    1650 – En curso
    Chaos Crags
  4. 980 (±300 años)VEI ?Estimación geológica
    980 – En curso
    Chaos Crags
  5. 880 (±300 años)VEI ?Estimación geológica
    880 – En curso
    Chaos Crags
  6. 800 (±300 años)VEI ?Estimación geológica
    800 – En curso
    Chaos Crags

Enlaces externos

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