πŸŒ‹VolcanoAtlas

Manam Volcano

Papua New Guinea's Most Dangerous Island Volcano

Elevation

1,807 m

Last Eruption

2018-present

Type

Stratovolcano

Country

Papua New Guinea

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 Activity8 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 Papua New Guinea

Interesting Facts

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Manam has produced four VEI 4 eruptions since 1919 β€” more than most volcanoes produce in centuries β€” making it one of the most violently active volcanoes in the southwestern Pacific.

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The entire population of Manam Island β€” approximately 10,000 people β€” has been evacuated at least three times since 2004, yet most islanders have returned each time.

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Manam's four radial valleys channel pyroclastic flows from the summit directly to the coast in minutes, creating a lethal funnel effect that leaves coastal villages in the direct firing line.

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The volcano's total height from the seafloor is approximately 4,000 m β€” more than double its above-water elevation of 1,807 m β€” making it a massive submarine mountain.

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In the 1996 eruption, pyroclastic flows killed 13 people who had no time to flee because the flows traveled from summit to coast faster than any warning system could operate.

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Manam has erupted 46 times since 1616, averaging roughly one eruption every 8-9 years, though activity has been nearly continuous since the mid-20th century.

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The 2004 evacuation created a displacement crisis lasting years, with evacuees in mainland camps facing inadequate shelter, food shortages, and social tension with host communities.

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Both of Manam's summit craters β€” the Main (northern) and Southern β€” are active, though the Southern crater has been the dominant eruptive vent for the past century.

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Five satellite volcanic cones near Manam's shoreline represent secondary vents, showing that eruptions have occurred at multiple points around the island throughout its history.

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Manam's persistent SO2 emissions are regularly detected by satellite instruments, making it one of the most visible volcanic degassing sources in the western Pacific.

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Papua New Guinea has 39 Holocene volcanoes β€” one of the highest concentrations of active volcanoes of any nation β€” and Manam is among the most dangerous.

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The Manam people have inhabited the island for centuries despite its volcanic activity, sustained by exceptionally fertile volcanic soils and rich surrounding fisheries.

Frequently Asked Questions

Is Manam Volcano currently erupting?
Yes, Manam has been in a state of semi-continuous eruption since 2018. Current activity includes Strombolian explosions, ash venting, and intermittent lava flows from the Southern crater. Occasional larger explosions produce ash columns reaching 5,000-10,000 m altitude. The volcano has produced three separate VEI 4 eruptions in the 21st century alone (2004, 2014, 2018). It is monitored by the Rabaul Volcanological Observatory and the Darwin Volcanic Ash Advisory Centre tracks its ash emissions for aviation safety.
Where is Manam Volcano?
Manam is a volcanic island in the Bismarck Sea, located 13 km off the northern coast of mainland Papua New Guinea in Madang Province. The island lies at approximately 4.08 degrees South, 145.04 degrees East. The nearest mainland town is Bogia, accessible by boat in 1-2 hours. Manam is part of the Bismarck Volcanic Arc, a chain of active volcanoes in the southwestern Pacific generated by the subduction of the Solomon Sea Plate beneath the Bismarck Plate.
How many people live on Manam Island?
Approximately 10,000 people live on Manam Island, concentrated in villages along the narrow coastal lowlands. The population is indigenous Manam people, Austronesian speakers who have inhabited the island for centuries. The population has been evacuated entirely on at least three occasions since 2004 due to major eruptions, but most residents have returned each time due to deep cultural attachment to their ancestral homeland and the lack of viable permanent resettlement options on the mainland. The population's continued residence on one of the world's most active volcanic islands is a major humanitarian concern.
Why is Manam so dangerous?
Manam is dangerous due to a combination of high eruption frequency, violent eruption style, and direct population exposure. The volcano has produced four VEI 4 eruptions since 1919 and erupts roughly every 8-9 years. Its four radial valleys channel pyroclastic flows from the summit directly to the coast in minutes β€” far too fast for evacuation. Approximately 10,000 people live in coastal villages at the base of these valleys, directly in the path of volcanic flows. The 1996 eruption killed 13 people because flows reached the coast before anyone could flee. Monitoring capabilities are limited compared to volcanoes in developed nations.
Has Manam been evacuated before?
Yes, Manam's entire population has been evacuated multiple times. The first complete evacuation occurred in 2004 when a VEI 4 eruption forced approximately 10,000 people to relocate to mainland camps near Bogia. Further evacuations occurred during the 2014 and 2018 eruptions. Each evacuation has followed a similar pattern: initial relocation to temporary mainland camps, deteriorating conditions in the camps, gradual return of islanders to Manam over months to years, and eventual re-eruption requiring another evacuation. The Manam displacement situation is considered one of the most challenging volcano-related humanitarian crises in the Pacific.
What type of volcano is Manam?
Manam is a stratovolcano (composite volcano) built primarily from basaltic to basaltic-andesitic lava flows and pyroclastic deposits. It forms a roughly circular island approximately 10 km in diameter, with a total edifice height of approximately 4,000 m from the seafloor (1,807 m above sea level). The volcano has two active summit craters and four distinctive radial valleys that channel eruptive products to the coast. Its eruption style ranges from persistent low-level Strombolian activity to violent VEI 4 paroxysms that generate pyroclastic flows, heavy tephra fall, and lava flows reaching the sea.
How tall is Manam Volcano?
Manam rises to 1,807 m (5,928 ft) above sea level. However, the total height of the volcanic edifice from the surrounding seafloor is approximately 4,000 m (13,100 ft), as the island is the summit of a much larger submarine mountain. Above water, the volcano presents a steep, conical profile divided into quadrants by four large radial valleys. For comparison among Papua New Guinea's volcanoes, Ulawun on New Britain is taller at 2,334 m (7,657 ft), but Manam's combination of height, isolation, and eruption frequency makes it distinctive.
When was Manam's worst eruption?
Manam's most destructive modern eruption occurred in October-November 2004, when VEI 4 explosions sent pyroclastic flows down the southeast and southwest valleys to the coast, killing at least 5 people and destroying coastal villages. The eruption forced the first-ever complete evacuation of all approximately 10,000 island residents. However, the 1996 eruption, while less explosive overall, was arguably more lethal per capita β€” 13 people were killed by pyroclastic flows that reached the coast before any evacuation was possible. The 1919 VEI 4 eruption was the first major documented paroxysm.