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United States · Stratovolcano

Kasuga Seamount

Kasuga 1

Type
Stratovolcano
Elevation
598m (submarine)
Last eruption
1959
Kasuga Seamount
Photo: NOAA · Public domain · Wikimedia Commons
Type
Stratovolcano
Country
United States
Region
Northwestern Pacific / Mariana Volcanic Arc
Elevation
598m (submarine)
Coordinates
21.765, 143.710
Last eruption
1959
Tectonic setting
Subduction zone / Crustal thickness unknown
Landform
Composite
Major rock type
Andesite / Basaltic andesite

Geological summary

Kasuga 1, the northernmost of three seamounts in the Kasuga seamount chain SE of Fukujin, rises from a depth of 3,000 m to within about 600 m of the ocean surface.

Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →

From Wikipedia

Kasuga 1 is a seamount and active volcano of the Mariana volcanic arc. It rises 3,000 m (9,800 ft) above the seafloor to about 600 m (2,000 ft) beneath the ocean surface. The volcano represents the northernmost of the three that forms the Kasuga seamount chain and is located southeast of Fukujin. Its last confirmed eruption was in July 1959 which produced pumice and another possible eruption may have occurred in 1975 when discolored water was observed around the seamount. Based on the samples of basalt and andesite collected at the summit, it is the oldest of the seamounts.

Wikipedia · CC BY-SA · Read full article →

Eruption history

2 recordedGlossary

Record summary

Confirmed eruptions
1
Uncertain eruptions
1
Span of confirmed record
1959 – 1959
Largest confirmed eruption
VEI 0 (1959)
Confirmed eruptions since 1900
1
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
1959~1961 · 1 eruptions · max VEI 01973~1975 · 1 eruptions · max VEI 019591962196719701973

Detailed timeline

  1. 1975VEI 0Method not stated
    1975-11-16 – end unknown
    21.78 N 143.71 E
  2. 1959VEI 0Observed
    1959-07-15 – end unknown

Nearby volcanoes

External links

⚠ For reference only. Not for emergency response.