Mount Moffett
Moffett
Stratovolcano · United States · 1196m

- Type
- Stratovolcano
- Country
- United States
- Region
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Elevation
- 1196m
- Coordinates
- 51.944, -176.747
- Last eruption
- -1600
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
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.
From Wikipedia
Mount 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.
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Eruption history
Detailed timeline
- 1600 BCEVEI ?Geological estimateBCE 1600 – Ongoing
- 3750 BCEVEI ?Geological estimateBCE 3750 – Ongoing
- 7850 BCEVEI ?Geological estimateBCE 7850 – Ongoing
External links
⚠ For reference only. Not for emergency response.