Mount Aniakchak
Aniakchak
Kaldera · United States · 1341 m

- Tipe
- Kaldera
- Negara
- United States
- Wilayah
- North America Volcanic Regions / Alaska Peninsula Volcanic Arc
- Ketinggian
- 1341 m
- Koordinat
- 56.880, -158.170
- Letusan terakhir
- 1931
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisMount 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.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1942VEI ?Perkiraan geologi1942 – Berlangsung
- 1931VEI 4Teramati1931-05-01 – 1931-06-13West and SW caldera floor
- 1540 (±100 tahun)VEI 4Perkiraan geologi1540 – BerlangsungNW & S caldera floor (Half Cone, Vent Mtn)
- 1470 (±20 tahun)VEI ?Perkiraan geologi1470 – BerlangsungSE caldera floor (New Cone)
- 1370 (±55 tahun)VEI ?Perkiraan geologi1370 – BerlangsungNW caldera floor (Half Cone)
- 1280 (±145 tahun)VEI ?Perkiraan geologi1280 – BerlangsungNW caldera floor (Half Cone)
- 1190 (±30 tahun)VEI ?Perkiraan geologi1190 – BerlangsungNW caldera floor (Half Cone)
- 1120 (±80 tahun)VEI ?Perkiraan geologi1120 – BerlangsungEast-central caldera (Surprise Cone)
- 1050VEI ?Perkiraan geologi1050 – BerlangsungVent Mtn and other vents?
- 700 (±250 tahun)VEI 0Perkiraan geologi700 – BerlangsungS & NW caldera floor (Vent Mtn & Half Cone)
- 460VEI ?Perkiraan geologi460 – Berlangsung
- 200 (±255 tahun)VEI ?Perkiraan geologi200 – BerlangsungNorthern & western caldera floor
- 370 SM (±210 tahun)VEI ?Perkiraan geologiBCE 370 – Berlangsung
- 1645 SM (±10 tahun)VEI 6Perkiraan geologiBCE 1645 – Berlangsung
- 2550 SM (±500 tahun)VEI ?Perkiraan geologiBCE 2550 – Berlangsung
- 5930 SM (±240 tahun)VEI ?Perkiraan geologiBCE 5930 – Berlangsung
- 6300 SM (±1250 tahun)VEI 6Perkiraan geologiBCE 6300 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.