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Philippines · Stratovolcano

Camiguin

Type
Stratovolcano
Elevation
1552m
Last eruption
1953
Camiguin
Photo: justDONQUE.images · CC BY 2.0 · Wikimedia Commons
Type
Stratovolcano
Country
Philippines
Region
Western Pacific / Mindanao Volcanic Province
Elevation
1552m
Coordinates
9.203, 124.673
Last eruption
1953
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic andesite

Geological summary

The 20-km-long Camiguin Island just off the coast of north-central Mindanao Island consists of four overlapping stratovolcanoes overlying older buried edifices.

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

From Wikipedia

Summary of the Wikipedia article “Camiguin”

Camiguin, officially the Province of Camiguin, is an island province in the Philippines located in the Bohol Sea, about 10 kilometers (6.2 mi) off the northern coast of mainland Mindanao. It is geographically part of Region X, the Northern Mindanao Region of the country and formerly a part of Misamis Oriental province.

Wikipedia · CC BY-SA · Read full article →

Eruption history

4 recordedGlossary

Record summary

Confirmed eruptions
4
Uncertain eruptions
0
Span of confirmed record
1827 – 1953
Largest confirmed eruption
VEI 3 (1948)
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
1827~1839 · 1 eruptions · max VEI 21851~1863 · 1 eruptions · max VEI 21863~1875 · 1 eruptions · max VEI 21936~1948 · 1 eruptions · max VEI 318271851188819121936

Detailed timeline

  1. 1948VEI 3Observed
    1948-09-01 – 1953-07-16
    Upper NE flank of Hibok-Hibok
  2. 1871VEI 2Observed
    1871-04-30 – 1875-07-02
    Lower NW flank of Hibok-Hibok (Mt. Vulcan)
  3. 1862VEI 2Observed
    1862-07-02 – end unknown
    Hibok-Hibok
  4. 1827VEI 2Observed
    1827-07-02 – end unknown
    Hibok-Hibok

Nearby volcanoes

External links

⚠ For reference only. Not for emergency response.