Narcondum

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 13.43°N
  • 94.28°E

  • 710 m
    2329 ft

  • 260001
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Narcondum.



 Available Weekly Reports

There are no Weekly Reports available for Narcondum.

There are no Holocene eruptions known for Narcondum. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

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.

Krishnan M S, 1957. Volcanic episodes in Indian geology. J Madras Univ, 27: 193-209.

Mallet F R, 1895. Some early allusions to Barren Island; with a few remarks thereon. Geol Surv India Mem, 28(1): 22-34.

Pal T, Mitra S K, Sengupta S, Katari A, Bandopadhyay P C, Bhattacharya A K, 2007. Dacite--andesites of Narcondam volcano in the Andaman Sea -- an imprint of magma mixing in the inner arc of the Andaman--Java subduction system. J Volc Geotherm Res, 168: 93-113.

Raina V K, 1987. A note on sulfur occurrence in the volcanoes of Bay of Bengal. Indian Minerals, 41: 79-86.

Shanker R, Haldar D, Absar A, Chakraborty S C, 2001. Pictorial Monograph of the Barren Island Volcano. Kolkata: Geol Surv India, 87 p.

Narcondum volcano, an island possession of India in the Andaman Sea, is part of a volcanic arc that continues northward from Sumatra to Burma (Myanmar). The small 3 x 4 km wide conical island, located about 130 km east of North Andaman Island, rises to 710 m, but its base lies an additional 1000 m beneath the sea. The island is densely vegetated, bounded by cliffs on the southern side, and capped by three peaks. No evidence of historical volcanism is present, although the summit region is less densely vegetated. Volcanism at the andesitic volcano is considered to have continued into the Holocene (Krishnan, 1957). The island's name means "pit of hell," although the name could have been mistakenly transferred from the historically active Barren Island volcano, 140 km to the SSW.