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Dominica · Stratovolcano

Morne Plat Pays

Plat Pays, Morne

Type
Stratovolcano
Elevation
940m
Last eruption
1270
Morne Plat Pays
Photo: Lee Siebert (Smithsonian Institution) · Public domain · Wikimedia Commons
Type
Stratovolcano
Country
Dominica
Region
Middle America & Caribbean / Lesser Antilles Volcanic Arc
Elevation
940m
Coordinates
15.255, -61.341
Last eruption
1270
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Composite
Major rock type
Dacite

Geological summary

The Morne Plat Pays volcanic complex occupies the southern tip of the island of Dominica and has been active throughout the Holocene.

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

From Wikipedia

Morne Plat Pays is a volcano on the island of Dominica. Located on the southern region of the island, the volcano last erupted around the year 1270 AD. Since the mid-18th century, a number of earthquake swarms have occurred near the mountain, but these are not related to Morne Plat Pays' eruptive activity.

Wikipedia · CC BY-SA · Read full article →

Eruption history

4 recordedGlossary

Record summary

Confirmed eruptions
4
Uncertain eruptions
0
Span of confirmed record
4740 BCE – 1270
Largest confirmed eruption
No VEI recorded
Confirmed eruptions since 1900
0
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
4740 BCE~4540 BCE · 1 eruptions · max VEI ?533 BCE~333 BCE · 1 eruptions · max VEI ?268~469 · 1 eruptions · max VEI ?1070~1270 · 1 eruptions · max VEI ?4740 BCE3338 BCE1735 BCE333 BCE1070

Detailed timeline

  1. 1270 (±50 yrs)VEI ?Geological estimate
    1270 – end unknown
    Morne Patates
  2. 390 (±40 yrs)VEI ?Geological estimate
    390 – end unknown
    Morne Patates
  3. 430 BCEVEI ?Geological estimate
    430 BCE – end unknown
    Morne Patates ?
  4. 4740 BCEVEI ?Geological estimate
    4740 BCE – end unknown
    Morne Plat Pays

Nearby volcanoes

External links

⚠ For reference only. Not for emergency response.