Ile des Cendres

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 10.158°N
  • 109.014°E

  • -20 m
    -66 ft

  • 275060
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Ile des Cendres.



 Available Weekly Reports

There are no Weekly Reports available for Ile des Cendres.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1923 Mar 2 1923 May 13 Confirmed 2 Historical Observations

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Bondarenko V I, Nadezhnyi A M, 1985. Main structural features and morphology of the volcanic zone and individual submarine volcanoes in the vicinity of the Catwic-Phu Quy islands on the Vietnamese shelf as revealed by continuous seismic profiling data. Volc Seism, 1985(5): 34-43 (English translation 1989, 7: 701-716).

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Markov Y D, 1994. Recent sedimentogenesis on the Ile des Cendres volcanoes and adjacent shelf, South China Sea. Volc Seism, 15: 565-578 (English translation).

Neumann van Padang M, 1953. Philippine Islands and Cochin China. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 2: 1-49.

Patte E, 1925. Etude de l'Ile des Cendres, volcan apparu au large de la Cote d'Annam. Bull Serv Geol Indochina, 13: 5-19.

The Ile des Cendres group of submarine volcanoes off the SE coast of Vietnam consists of two submarine cinder cones that formed ephemeral islands during an eruption in 1923 and two submarine lava cones of uncertain age. The 1923 eruption produced two small islands, one about 30 m high and about 450 m long, and the other only 30 m wide and 30 cm high. A third submarine cone reached to within 20 m of the surface. Additional submarine cones occur between Ile des Cendres and the Vietnam mainland (Bondarenko and Nadezhnyi, 1989).