Morne Plat Pays

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 15.255°N
  • 61.341°W

  • 940 m
    3083 ft

  • 360110
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Morne Plat Pays.



 Available Weekly Reports

There are no Weekly Reports available for Morne Plat Pays.

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

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1270 ± 50 years Unknown Confirmed   Radiocarbon (uncorrected) Morne Patates
0390 ± 40 years Unknown Confirmed   Radiocarbon (uncorrected) Morne Patates
0430 BCE (?) Unknown Confirmed   Radiocarbon (uncorrected) Morne Patates ?
4740 BCE (?) Unknown Confirmed   Radiocarbon (uncorrected) Morne Plat Pays

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.

Deplus C, Le Friant A, Boudon G, Komorowski J-C, Villemant B, Harford C, Segoufin J, Cheminee J-L, 2001. Submarine evidence for large-scale debris avalanches in the Lesser Antilles arc. Earth Planet Sci Lett, 192: 145-157.

Halama R, Boudon G, Villemant B, Joron J-L, Le Friant A, Komorowski J-C, 2006. Pre-eruptive crystallization conditions of mafic and silicic magmas at the Plat Pays volcanic complex, Dominica (Lesser Antilles). J Volc Geotherm Res, 153: 200-220.

Lindsay J M, Smith A L, Roobol M J, Stasiuk M V, 2005b. Dominica. In: Lindsay J M, Robertson R E A, Shepherd J B, Ali S (eds). {Volcanic Hazard Atlas of the Lesser Antilles}, Trinidad and Tobago, Seismic Res Unit, Univ West Indies, p 1-47.

Lindsay J M, Stasiuk M V, Shepherd J B, 2003. Geological history and potential hazards of the late-Pleistocene to Recent Plat Pays volcanic complex, Dominica, Lesser Antilles. Bull Volc, 65: 201-220.

Lindsay J M, Trumbull R B, Siebel W, 2005c. Geochemistry and petrogenesis of late Pleistocene to Recent volcanism in southern Dominica, Lesser Antilles. J Volc Geotherm Res, 148: 253-294.

Robson G R, Tomblin J, 1966. West Indies. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 20: 1-56.

Roobol M J, Wright J V, Smith A L, 1983. Calderas of gravity-slide structures in the Lesser Antilles Island Arc?. J Volc Geotherm Res, 19: 121-134.

Samper A, Quidelleur X, Boudon G, Le Friant A, Komorowski J C, 2008. Radiometric dating of three large volume flank collapses in the Lesser Antilles arc. J Volc Geotherm Res, 176: 485-492.

Seismic Research Unit, 2001. Seismo-volcanic activity in Dominica (updated July 11, 2001). Seismic Res Unit, Univ West Indies (http://www.uwiseismic.com/dominica.html).

Shepherd J B, 2001. Volcanoes of the eastern Caribbean: past activity and future hazards. Paper presented at the Workshop on Volcanic and Seismic Hazards in the eastern Caribbean, May 28- June 1, 2001, 57 p.

Shepherd J B, 1989. Eruptions, eruption precursors and related phenomena in the Lesser Antilles. In: Latter J H (ed), {Volcanic Hazards - Assessment and Monitoring}, Berlin: Springer-Verlag, p 292-311.

Wadge G, 1985. Morne Patates volcano, southern Dominica, Lesser Antilles. Geol Mag, 122: 253-260.

The Morne Plat Pays volcanic complex occupies the southern tip of the island of Dominica and has been active throughout the Holocene. An arcuate caldera that formed about 39,000 years ago as a result of a major explosive eruption and flank collapse is open to Soufrière Bay on the west. This depression cuts the SW side of Morne Plat Pays stratovolcano and extends to the southern tip of Dominica. At least a dozen small post-caldera lava domes were emplaced within and outside this depression, including one submarine dome south of Scotts Head. The latest dated eruptions occurred from the Morne Patates lava dome about 1270 CE, although younger deposits have not yet been dated. The Morne Plat Pays complex is the site of extensive fumarolic activity, and at least ten swarms of small-magnitude earthquakes, none associated with eruptive activity, have occurred since 1765 at Morne Patates.