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Yunaska Island

Yunaska

Gunung api perisai · United States · 550 m

The summit caldera rim of Yunaska is seen from an older volcanic center on the western side of the island. The younger eastern complex contains two nested calderas. A young lava flow to the far right descended through a notch in the caldera rim. The peaks in the background are (left-to-right) of Carlisle, Cleveland, and Herbert volcanoes.
The summit caldera rim of Yunaska is seen from an older volcanic center on the western side of the island. The younger eastern complex contains two nested calderas. A young lava flow to the far right descended through a notch in the caldera rim. The peaks in the background are (left-to-right) of Carlisle, Cleveland, and Herbert volcanoes. · Foto: Photo by Jim Meyers, 1992 (University of Wyoming, courtesy of Alaska Volcano Observatory). · Wikimedia Commons
Tipe
Gunung api perisai
Negara
United States
Wilayah
North America Volcanic Regions / Aleutian Ridge Volcanic Arc
Ketinggian
550 m
Koordinat
52.639, -170.632
Letusan terakhir
1937
Kondisi tektonik
Subduction zone / Intermediate crust (15-25 km)
Bentuk lahan
Shield
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

The elongated 9 x 23 km Yunaska in the Islands of the Four Mountains group of the Aleutian Islands is comprised of two distinct volcanic centers. The older western center consists of the eroded remnants of four overlapping stratovolcanoes that form a linear, NNE-trending ridge. Cinder cones and fissure-fed lava flows extend from the western end of the complex. The younger eastern complex consists of a shield volcano capped by two nested calderas. The 3.5-km-wide Coats caldera is located within an older 10 x 13 km caldera and contains cinder cones and a lava field. Two areas of youthful lava flows extend down the flank through a gap in the SW caldera rim and cover the upper N flank of the caldera. Vents are found on the flanks of the caldera within a kilometer of its rim. A post-caldera cone is capped by a small summit crater. The eastern center is presumably the source of eruptions recorded since the early 1800s.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1817~1829 · 2 letusan · VEI maks. 31829~1841 · 1 letusan · VEI maks. 21865~1877 · 1 letusan · VEI maks. 21925~1937 · 2 letusan · VEI maks. 318171841187719011925

Garis waktu rinci

  1. 1937VEI 3Teramati
    1937-11-03 – 1937-11-04
  2. 1929VEI ?Perkiraan geologi
    1929 – Berlangsung
  3. 1873VEI 2Perkiraan geologi
    1873 – Berlangsung
  4. 1830VEI 2Teramati
    1830 – Berlangsung
  5. 1824VEI 3Teramati
    1824 – Berlangsung
  6. 1817VEI ?Perkiraan geologi
    1817 – Berlangsung

Tautan eksternal

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