Mount Aniakchak
Aniakchak
Caldera · United States · 1341m

- Type
- Caldera
- Country
- United States
- Region
- North America Volcanic Regions / Alaska Peninsula Volcanic Arc
- Elevation
- 1341m
- Coordinates
- 56.880, -158.170
- Last eruption
- 1931
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
One of the most dramatic calderas of the Aleutian arc, the 10-km-wide Aniakchak caldera formed around 3,400 years ago during a voluminous eruption in which pyroclastic flows traveled more than 50 km N to the Bering Sea and also reached the Pacific Ocean to the south. At least 40 explosive eruptions have been documented during the past 10,000 years, making it the most active volcano of the eastern Aleutian arc. A dominantly andesitic pre-caldera volcano was constructed above basement Mesozoic and Tertiary sedimentary rocks that are exposed in the caldera walls to elevations of about 610 m. The ice-free caldera floor contains many pyroclastic cones, tuff cones, maars, and lava domes. Surprise Lake on the NE side drains through The Gates, a steep-walled breach on the east side of the 1-km-high caldera rim that was the site of catastrophic draining of a once larger lake about 1850 years BP. Vent Mountain and Half Cone are two long-lived vents on the south-central and NW caldera floor, respectively. The first and only confirmed historical eruption took place in 1931 from vents on the west and SW caldera floor.
From Wikipedia
Mount Aniakchak is a volcano on the western Alaska Peninsula. Part of the Aleutian Volcanic Arc, it was formed by the subduction of the oceanic Pacific Plate under the North American Plate. Aniakchak is a 10 kilometers (6.2 mi) wide caldera with a break to the northeast. The caldera contains Surprise Lake and many volcanic cones, maars and craters, including Vent Mountain. The volcano has erupted mainly calc-alkaline rocks ranging from basalt to rhyolite.
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Eruption history
Detailed timeline
- 1942VEI ?Geological estimate1942 – Ongoing
- 1931VEI 4Observed1931-05-01 – 1931-06-13West and SW caldera floor
- 1540 (±100 yrs)VEI 4Geological estimate1540 – OngoingNW & S caldera floor (Half Cone, Vent Mtn)
- 1470 (±20 yrs)VEI ?Geological estimate1470 – OngoingSE caldera floor (New Cone)
- 1370 (±55 yrs)VEI ?Geological estimate1370 – OngoingNW caldera floor (Half Cone)
- 1280 (±145 yrs)VEI ?Geological estimate1280 – OngoingNW caldera floor (Half Cone)
- 1190 (±30 yrs)VEI ?Geological estimate1190 – OngoingNW caldera floor (Half Cone)
- 1120 (±80 yrs)VEI ?Geological estimate1120 – OngoingEast-central caldera (Surprise Cone)
- 1050VEI ?Geological estimate1050 – OngoingVent Mtn and other vents?
- 700 (±250 yrs)VEI 0Geological estimate700 – OngoingS & NW caldera floor (Vent Mtn & Half Cone)
- 460VEI ?Geological estimate460 – Ongoing
- 200 (±255 yrs)VEI ?Geological estimate200 – OngoingNorthern & western caldera floor
- 370 BCE (±210 yrs)VEI ?Geological estimateBCE 370 – Ongoing
- 1645 BCE (±10 yrs)VEI 6Geological estimateBCE 1645 – Ongoing
- 2550 BCE (±500 yrs)VEI ?Geological estimateBCE 2550 – Ongoing
- 5930 BCE (±240 yrs)VEI ?Geological estimateBCE 5930 – Ongoing
- 6300 BCE (±1250 yrs)VEI 6Geological estimateBCE 6300 – Ongoing
External links
⚠ For reference only. Not for emergency response.