🌋VolcanoAtlas

Soufrière Hills

The Volcano That Buried a Capital City

Elevation

915 m

Last Eruption

2013

Type

Complex Stratovolcano

Country

United Kingdom (Montserrat)

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskLow
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Unknown
Silica Content
Varied composition

Tectonic Setting

Unknown
Intraplate setting with hotspot or regional volcanic activity.

Age & Formation

Epoch
Unknown
Evidence
Unknown

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity13 years agoRecentRecently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Watch
Dormant but monitored. Capable of renewed activity.

Interesting Facts

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Plymouth, Montserrat's capital, is the only ghost town in the world that serves as the official capital of a political territory — it remains the de jure capital despite being buried under meters of volcanic debris.

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The 1995–2013 eruption produced over 1 km³ of andesitic magma, making it one of the most voluminous dome-building eruptions of the modern era.

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Nineteen people were killed on June 25, 1997, when a dome-collapse pyroclastic flow swept through the officially evacuated zone — they had returned to their homes against evacuation orders.

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Approximately two-thirds of Montserrat's population (roughly 7,000 of 12,000 people) fled the island, with 4,000 relocating to the United Kingdom.

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The eruption destroyed W. H. Bramble Airport and AIR Studios Montserrat, where artists including The Police, Dire Straits, and Elton John had recorded music.

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Scientists discovered two interconnected magma chambers beneath Soufrière Hills — at 6 km and 12 km depth — explaining the sustained decades-long magma supply.

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The Montserrat Volcano Observatory has maintained continuous monitoring since 1995, producing one of the most comprehensive datasets of any dome-building eruption in history.

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The southern half of Montserrat remains a designated Exclusion Zone — one of the most restrictive volcanic access prohibitions in the world.

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Before the 1995 eruption, Soufrière Hills had not erupted in recorded history — the last activity was likely around 1550 CE, before English colonization in 1632.

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A May 2006 dome collapse sent 90 million cubic meters of material into the Caribbean Sea within three hours — the entire lava dome destroyed in a single event.

Frequently Asked Questions

Is Soufrière Hills still active?
Yes, Soufrière Hills remains an active volcano. The eruptive episode that began in 1995 produced its last confirmed activity in 2013. While seismicity and gas emissions have declined since 2010, the Montserrat Volcano Observatory continues comprehensive monitoring. The Scientific Advisory Committee classifies the volcano as capable of reactivation with limited warning. The southern Exclusion Zone remains in effect, and Plymouth is still off-limits. Volcanologists emphasize that dome-building volcanoes can resume activity after years of apparent quiescence.
What happened to Plymouth, Montserrat?
Plymouth, the capital of Montserrat, was progressively destroyed by the Soufrière Hills eruption between 1995 and 1997. The city was first evacuated in August 1995, then permanently evacuated in April 1996. In August 1997, pyroclastic flows swept through the city, burying buildings under more than 12 meters of volcanic mud and ash. Today, Plymouth is a ghost town within the Exclusion Zone — rooftops and upper floors of some buildings remain visible above the debris. It remains the de jure capital of Montserrat, though the government operates from Brades in the north.
How many people died in the Montserrat eruption?
Nineteen people were killed during the Soufrière Hills eruption, all on June 25, 1997, when a massive dome-collapse pyroclastic flow swept down the northeastern flank of the volcano. The victims were in the officially evacuated Streatham village area, having returned to their homes. No other fatalities directly resulted from the eruption, largely due to the effective, if difficult, evacuation of the southern half of the island. The relatively low death toll (compared to the scale of destruction) is credited to the monitoring and evacuation efforts by the MVO and Montserrat government.
Can you visit Montserrat?
Yes, Montserrat is accessible by ferry from Antigua (approximately 90 minutes) and by small aircraft to John A. Osborne Airport. The northern third of the island is inhabited and safe for visitors, offering Caribbean charm with lush hiking trails, black-sand beaches, and views of the volcano. Guided tours approach the edge of the Exclusion Zone, and the MVO observation post at Jack Boy Hill provides panoramic views of the devastated southern landscape and the lava dome. The Montserrat Volcano Observatory offers educational presentations about the eruption.
What type of volcano is Soufrière Hills?
Soufrière Hills is classified as a complex stratovolcano, specifically an andesitic lava dome complex. Its eruptions are characterized by the extrusion of viscous andesitic lava that forms steep-sided domes within the summit crater. These domes grow slowly over months to years, then collapse catastrophically under their own weight, generating deadly pyroclastic density currents. This eruption pattern — dome growth punctuated by explosive collapse — is typical of subduction-zone andesitic volcanoes and is among the most hazardous volcanic behaviors.
Will Soufrière Hills erupt again?
Future eruptions at Soufrière Hills are considered highly likely. The volcano's twin magma chambers at 6 km and 12 km depth represent a substantial reservoir capable of sustaining further activity. While the current eruptive episode appears to be waning (declining seismicity and gas flux since 2010), the volcano's history shows multi-century repose periods followed by renewed activity. The Montserrat Volcano Observatory maintains continuous monitoring specifically because reactivation could occur with limited warning. The southern Exclusion Zone will remain in effect for the foreseeable future.