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Gareloi Volcano

Gareloi

Stratovolkan · United States · 1573 m

Gareloi in the western Aleutian Islands is seen here from the S. This photo shows lava flows with clear levees from a 1980s eruption. The 8 x 10 km diameter Gareloi Island consists of a stratovolcano with two peaks and a SE-trending fissure that formed during a 1929 eruption and extends  to the sea.
Gareloi in the western Aleutian Islands is seen here from the S. This photo shows lava flows with clear levees from a 1980s eruption. The 8 x 10 km diameter Gareloi Island consists of a stratovolcano with two peaks and a SE-trending fissure that formed during a 1929 eruption and extends to the sea. · Foto: Photo by Game McGimsey, 2003 (Alaska Volcano Observatory, U.S. Geological Survey). · Wikimedia Commons
Tipe
Stratovolkan
Negara
United States
Wilayah
North America Volcanic Regions / Aleutian Ridge Volcanic Arc
Ketinggian
1573 m
Koordinat
51.790, -178.794
Letusan terakhir
1989
Kondisi tektonik
Subduction zone / Intermediate crust (15-25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The 8 x 10 km Gareloi Island, the northernmost volcano of the Delarof Group at the western end of the Andreanof Islands, consists of a stratovolcano with two summits and a prominent SE-trending fissure. The fissure was formed during an eruption in 1929 and extends from the southern summit to the sea. Steep sea cliffs that are cut into rocks of an older, eroded center are found on the SW coast, and submarine deposits of three debris avalanches produced by edifice collapse are found offshore. Young lava flows cover the older volcano from the summit to the coast along three broad axes trending NW, ENE, and S. The 1929 eruption originated from 13 craters along a 4-km-long fissure. Phreatic explosions were followed by the ejection of glassy pumice, lapilli, scoria, and older blocks, as well as by the emission of four short, steep lava flows, one of which reached the SE coast.

Ringkasan Wikipedia

Ringkasan Inggris

Mount Gareloi, or Gareloi Volcano, is a stratovolcano in the Aleutian Islands of Alaska, United States, about 1,259 miles (2,026 km) from Anchorage. Gareloi is located on Gareloi Island, and comprises most of its land mass. The island also has two small glaciers which protrude to the northwest and southeast.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1760~1784 · 1 letusan · VEI maks. ?1784~1807 · 3 letusan · VEI maks. 21807~1831 · 1 letusan · VEI maks. 21854~1878 · 1 letusan · VEI maks. 21902~1925 · 1 letusan · VEI maks. 31925~1949 · 2 letusan · VEI maks. 31949~1972 · 2 letusan · VEI maks. 21972~1996 · 5 letusan · VEI maks. 317601807187819251972

Garis waktu rinci

  1. 1996VEI 1Perkiraan geologi
    1996-09-27 – Berlangsung
  2. 1989VEI 1Teramati
    1989-08-17 – 1989-08-17
  3. 1987VEI 1Teramati
    1987-08-30 – 1987-09-04
    N crater rim, E flank
  4. 1982VEI 3Teramati
    1982-01-15 – 1982-01-15
  5. 1980VEI 3Teramati
    1980-08-07 – 1980-09-17
  6. 1952VEI 2Teramati
    1952-01-17 – Berlangsung
  7. 1950VEI 1Teramati
    1950-07-02 – 1951-07-02
  8. 1929VEI 3Teramati
    1929-04 – 1930
    SE flank fissure (near summit to sea)
  9. 1927VEI ?Perkiraan geologi
    1927 – Berlangsung
  10. 1922VEI 3Teramati
    1922 – Berlangsung
  11. 1873VEI 2Teramati
    1873 – Berlangsung
  12. 1828VEI 2Perkiraan geologi
    1828 – 1829
  13. 1792VEI 2Teramati
    1792 – Berlangsung
  14. 1791VEI 2Teramati
    1791 – Berlangsung
  15. 1790VEI 2Teramati
    1790 – Berlangsung
  16. 1760VEI ?Perkiraan geologi
    1760 – Berlangsung

Tautan eksternal

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