Mount Moffett
Moffett
Estratovolcán · United States · 1196 m

- Tipo
- Estratovolcán
- País
- United States
- Región
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Altitud
- 1196 m
- Coordenadas
- 51.944, -176.747
- Última erupción
- -1600
- Contexto tectónico
- Subduction zone / Intermediate crust (15-25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
Resumen geológico
Rising above Adak, the largest town of the Aleutians, Mount Moffett is a modest-sized, eroded stratovolcano with several flank lava domes. The summit cone has been largely destroyed by glacial erosion, and has been filled by an andesitic plug dome. Five other lava domes are scattered over the flanks of the volcano. The south flank lava dome is one of the youngest features of the northern Adak Island volcanoes. The Heart Lake lava flow west of Sweeper Cove on the SE side of the volcano is another young volcanic feature. Several Holocene ash layers on Adak Island have been attributed to Moffett volcano. Its proximity to Adak Naval Air Station makes this one of the most accessible of the Aleutian volcanoes. Kiguga Warm Springs are located at Cape Kiguga, west of Mount Moffet, and the northern part of Adak Island has been investigated for geothermal power production.
Resumen de Wikipedia
Resumen en inglésMount Moffett is a mountainous stratovolcano that forms the summit of Adak Island of the Aleutian Islands in the U.S. state of Alaska. Its peak reaches 3,924 feet (1,196 m). It is heavily glaciated and is made primarily of high alumina basalt and andesite. It has never had an eruption in recorded history. The southern flank of the mountain is assumed to be its youngest side. In comparison to other Aleutian stratovolcanoes, Moffett is a small vent, characteristic of its mixed composition.
Wikipedia · CC BY-SA · Leer artículo completo →
Historial de erupciones
Línea de tiempo detallada
- 1600 a. C.VEI ?Estimación geológicaBCE 1600 – En curso
- 3750 a. C.VEI ?Estimación geológicaBCE 3750 – En curso
- 7850 a. C.VEI ?Estimación geológicaBCE 7850 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.