πŸŒ‹VolcanoAtlas

Ambae

The Pacific's Most Voluminous Island Shield Volcano

Elevation

1,496 m

Last Eruption

2025

Type

Shield

Country

Vanuatu

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Lava flows and fountaining
  • Volcanic gas emissions
  • Local explosive activity

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 Activity1 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Active
Recent volcanic activity detected. Continuous monitoring in place.

Other Volcanoes in Vanuatu

Interesting Facts

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Ambae is the most voluminous volcano in the New Hebrides arc at approximately 2,500 km3 β€” the vast majority of this volume lies beneath the Pacific Ocean.

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The 2017-2018 eruption forced the complete evacuation of all ~11,000 residents of Ambae, one of the largest volcanic evacuations in Pacific Island history.

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Ambae's summit contains three crater lakes β€” Manaro Ngoru, Voui, and Manaro Lakua β€” a rare triple-lake summit configuration among the world's active volcanoes.

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Lake Voui changes color dramatically during eruptions, shifting from blue-green to red, gray, or brown depending on volcanic gas input and suspended sediment.

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Ambae has erupted seven times between 2005 and 2025, making it one of the most frequently active volcanoes in the southwestern Pacific during this period.

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Acid rain from Ambae's eruptions has repeatedly devastated the island's vegetation, turning tropical forests brown and poisoning rainwater collection systems β€” the island's primary freshwater source.

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A tuff cone built within Lake Voui first emerged as a small island during the 2005 eruption and has grown with each subsequent event.

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The Australian Plate subducts beneath the Pacific Plate at the New Hebrides Trench at approximately 9 cm per year β€” one of the fastest convergence rates on Earth β€” fueling Ambae's activity.

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Despite being classified as a shield volcano, Ambae produces explosive eruptions enhanced by magma-water interaction in the crater lakes (phreatomagmatic eruptions).

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The 2017-2018 evacuation displaced communities for months, causing food insecurity and social disruption as entire villages were relocated to neighboring islands.

Frequently Asked Questions

Is Ambae still erupting?
Ambae has been erupting frequently in recent years, with confirmed eruptions in 2017-2018, 2021, 2023 (two events), 2024, and 2025. While these are separate eruptive episodes rather than one continuous eruption, the high frequency of activity indicates that Ambae's magmatic system is highly active. The Vanuatu Meteorology and Geo-Hazards Department (VMGD) monitors the volcano continuously and adjusts alert levels as conditions change. Residents and visitors should check current status before travel.
Why was Ambae evacuated in 2017?
Ambae was evacuated in 2017-2018 because a VEI 3 eruption β€” the most powerful in the island's recorded history β€” produced heavy ashfall that contaminated water supplies, destroyed crops, and made air quality hazardous. The eruption from the summit Lake Voui area sent ash columns several kilometers high and generated acid rain that devastated vegetation across the island. The Vanuatu government ordered the complete evacuation of all approximately 11,000 residents, who were transported by boat to neighboring islands including Maewo, Pentecost, and Santo. The displacement lasted months.
How big is Ambae volcano?
Ambae is enormous. The visible island measures 16 x 38 km with a summit elevation of 1,496 m (4,908 ft), but the total volcano β€” including its submarine base β€” has a volume of approximately 2,500 km3, making it the most voluminous volcano in the entire New Hebrides volcanic arc. Most of this volume is hidden beneath the Pacific Ocean. By comparison, the island's surface area is about 400 km2. The submarine flanks descend thousands of meters to the ocean floor.
What type of volcano is Ambae?
Ambae is classified as a shield volcano, characterized by its broad, gently sloping profile built by successive eruptions of fluid basaltic lava. This is unusual for a volcano in a subduction zone setting, where stratovolcanoes are more common. Ambae's basaltic composition gives it lower-viscosity magma that tends to produce less explosive eruptions than silica-rich stratovolcanoes. However, the interaction between rising magma and the summit crater lakes creates phreatomagmatic explosions that can be significantly more violent than purely magmatic eruptions of the same magnitude.
What are the crater lakes on Ambae?
Ambae's summit contains three crater lakes: Manaro Ngoru, Lake Voui (also spelled Vui), and Manaro Lakua. Lake Voui is the central and most volcanically active of the three, hosting a tuff cone that has grown during successive eruptions since 2005. The lake changes color dramatically based on volcanic activity β€” shifting from blue-green during quiescence to red, gray, or brown during unrest as volcanic gases alter the water chemistry. The lakes sit within nested calderas at the summit of the shield volcano and serve as natural indicators of subsurface volcanic conditions.
Can you visit Ambae?
Ambae is accessible but not a conventional tourist destination. Small aircraft connect the island to Port Vila and Santo when the airstrip is operational, and inter-island boats provide alternative transport. Basic village accommodation is available on the coast. The summit crater lakes are a spectacular sight when volcanic activity permits safe access. However, visitors must check the current volcanic alert level with VMGD, as eruptions occur frequently and can escalate with little warning. Facilities on the island are minimal, and travel logistics require advance planning.