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Kasuga Seamount

Kasuga 1

Stratovolcano · United States · 598m (submarine)

Kasuga, the northernmost of three seamounts in the Kasuga seamount chain (and also known as Kasuga 1), rises to within about 600 m of the sea surface SE of Fukujin submarine volcano. A series of flank vents are located low on the southern side of the edifice. Pumice from a submarine eruption was witnessed in 1959.
Kasuga, the northernmost of three seamounts in the Kasuga seamount chain (and also known as Kasuga 1), rises to within about 600 m of the sea surface SE of Fukujin submarine volcano. A series of flank vents are located low on the southern side of the edifice. Pumice from a submarine eruption was witnessed in 1959. · Photo: Image courtesy of NOAA, 2003 (http://oceanexplorer.noaa.gov/explorations/03fire/logs/mar02/media/kasuga.html). · Wikimedia Commons
Type
Stratovolcano
Country
United States
Region
Northwestern Pacific Volcanic Regions / 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 the Kasuga seamount chain SE of Fukujin, rises from a depth of 3,000 m to within about 600 m of the ocean surface. A series of flank vents are located low on the southern side of the edifice. The summit does not have a caldera or display hydrothermal activity, and is largely covered by volcaniclastics. Altered basaltic and andesitic rocks dredged from the summit suggest that it is the oldest of the three seamounts, although delicately preserved lava flow lobes and toes from a flank eruption suggest a very youthful age. It is listed as an active volcano by the Japan Meteorological Agency, and floating pumice attributed to a submarine eruption was seen south of it in the summer of 1959. Water discoloration from a possible submarine eruption was reported near the seamount in November 1975.

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.

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1959~1961 · 1 eruptions · max VEI 01973~1975 · 1 eruptions · max VEI 019591962196719701973

Detailed timeline

  1. 1975VEI 0Geological estimate
    1975-11-16 – Ongoing
    21.78 N 143.71 E
  2. 1959VEI 0Observed
    1959-07-15 – Ongoing

External links

⚠ For reference only. Not for emergency response.