🌋VolcanoAtlas

Volcanoes in Papua New Guinea

39 Volcanoes Across the Bismarck and Bougainville Arcs

39
Total Volcanoes
22
Historically Active
Balbi
2,715 m
Tallest Volcano
2025
Ulawun / Bagana / Manam / Langila
Most Recent

Volcano Locations in Papua New Guinea

Showing 39 of 39 volcanoes
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Click any marker to view volcano details • 39 volcanoes total

Quick Stats

How Many Volcanoes?
Papua New Guinea has 39 Holocene volcanoes in the Smithsonian database, making it the seventh most volcanically active country on Earth and the most volcanic nation in the southwestern Pacific.
How Many Active?
At least 22 PNG volcanoes have confirmed historical eruptions. Ulawun (47), Manam (41), and Langila (26) are among the most frequently active volcanoes on Earth.
Why So Many Volcanoes?
PNG sits along multiple subduction zones where the Pacific, Solomon Sea, and South Bismarck plates converge, creating the Bismarck and Bougainville volcanic arcs.
Tallest Volcano
Balbi at 2,715 m (8,907 ft) on Bougainville Island
Most Recent Eruption
Ulawun, Bagana, Manam, and Langila in 2025

Overview

Papua New Guinea has 39 Holocene volcanoes catalogued by the Smithsonian Global Volcanism Program, making it the seventh most volcanically active country in the world and by far the most volcanically prolific nation in the southwestern Pacific. Despite having fewer volcanoes than countries like the [[country:united-states|United States]] (165) or [[country:japan|Japan]] (105), PNG punches far above its weight in eruption frequency: its 261 confirmed eruptions yield an average of nearly 7 eruptions per volcano — one of the highest ratios on Earth. Four PNG volcanoes are among the most active on the planet: [[volcano:ulawun|Ulawun]] (47 eruptions), [[volcano:manam|Manam]] (41 eruptions), [[volcano:langila|Langila]] (26 eruptions), and [[volcano:bagana|Bagana]] (25 eruptions).

The country’s volcanoes are distributed across several island arcs in the Bismarck Sea and Solomon Sea regions, with the island of New Britain hosting the densest concentration of active centers.

PNG’s volcanic history is punctuated by catastrophic events that rank among the largest in the Pacific during the Holocene. Eight eruptions have reached VEI 6 — a remarkably high count for a single country — including the devastating ~1660 CE Long Island eruption and the ~683 CE Rabaul caldera collapse. The 1951 eruption of [[volcano:lamington|Lamington]] killed nearly 3,000 people and was one of the deadliest volcanic disasters of the 20th century.

The 1994 [[volcano:rabaul|Rabaul]] eruption forced the evacuation of the entire city of Rabaul (population ~17,000), transforming the former provincial capital into a ghost town buried under meters of ash. Today, monitoring is conducted by the Rabaul Volcanological Observatory (RVO), which watches over this exceptionally active volcanic landscape with limited but dedicated resources. PNG’s volcanoes sit squarely within the [[special:ring-of-fire|Ring of Fire]], along one of its most complex tectonic junctions.

Why Png Has Volcanoes

Papua New Guinea’s intense volcanic activity is the product of one of the most tectonically complex convergent plate boundaries on Earth. The country sits at the collision zone of multiple microplates — the Pacific, Solomon Sea, South Bismarck, and North Bismarck plates — all interacting with the Indo-Australian Plate. This complex mosaic of subduction zones, transform faults, and spreading centers generates more volcanic arcs per unit area than almost any other region on the planet.

The primary volcanic arc is the Bismarck Volcanic Arc, extending along the northern coast of New Britain and westward through the Bismarck Sea. This arc is generated by the northward subduction of the Solomon Sea Plate beneath the South Bismarck Plate. Ulawun, Rabaul, Langila, and most of New Britain’s volcanoes belong to this system.

The Bougainville Volcanic Arc runs through Bougainville Island where the Pacific Plate subducts westward. Bagana, Balbi, Billy Mitchell, and Loloru sit on this arc.

Convergence rates in the PNG region are among the highest on Earth — the Pacific Plate moves westward at approximately 10 cm per year relative to the Indo-Australian Plate. The Solomon Sea Plate subducts at 7–10 cm per year. These rapid rates drive high magma production and correspondingly frequent eruptions.

The crust beneath PNG’s arcs is predominantly oceanic to transitional (15–25 km thick), which allows basaltic to andesitic magmas to reach the surface more readily than through thick continental crust. This explains the predominantly andesitic compositions of PNG’s arc volcanoes, compared to the more evolved dacitic and rhyolitic compositions common in continental-arc countries like [[country:chile|Chile]].

Major Volcanoes

**Rabaul** — [[volcano:rabaul|Rabaul]] caldera on the northeastern tip of New Britain is PNG’s most historically significant volcanic center. The 688-m-high asymmetrical shield contains a broad harbor — actually a flooded caldera — that served as the island’s largest city until 1994, when simultaneous eruptions from Vulcan and Tavurvur buried much of the town. The caldera has 19 confirmed eruptions and a VEI max of 6, including a massive caldera-forming eruption around 683 CE.

**Ulawun** — [[volcano:ulawun|Ulawun]], known locally as ‘The Father,’ is the tallest volcano in the Bismarck arc at 2,334 m (7,657 ft) and one of PNG’s most frequently active with 47 confirmed eruptions. This symmetrical [[special:types-of-volcanoes|stratovolcano]] is designated a Decade Volcano due to its explosive history and proximity to populated areas. It erupted most recently in 2025.

**Manam** — [[volcano:manam|Manam]] is a 10-km-wide volcanic island 13 km off the mainland coast and one of PNG’s most dangerous volcanoes. With 41 confirmed eruptions including three VEI 4 events (1919, 2004, 2014), Manam has repeatedly displaced its island population. The 2004 eruption forced evacuation of all ~9,000 residents, many of whom remain displaced.

**Bagana** — [[volcano:bagana|Bagana]] on Bougainville is one of the youngest and most continuously active volcanoes in PNG. This 1,855-m lava cone may have built its entire edifice in approximately 300 years through persistent andesitic lava extrusion. With 25 confirmed eruptions and ongoing 2025 activity, Bagana produces persistent lava flows, Vulcanian explosions, and pyroclastic flows.

**Lamington** — [[volcano:lamington|Lamington]]’s January 21, 1951, eruption was one of the deadliest volcanic disasters of the 20th century. The VEI 4 Plinian eruption generated pyroclastic flows that devastated 230 km², killing approximately 2,942 people. The eruption was especially lethal because Lamington was not recognized as active beforehand.

**Long Island** — This volcanic complex hosts a massive 10 × 12.5 km caldera now filled by Lake Wisdom. The ~1660 CE eruption (VEI 6) was one of the largest volcanic events in the Pacific during the last millennium. With 11 confirmed eruptions including two VEI 6 events, Long Island demonstrates PNG’s capacity for truly catastrophic events.

**Langila** — One of New Britain’s most frequently active volcanoes with 26 confirmed eruptions through 2025. Four overlapping composite cones produce persistent Strombolian to Vulcanian eruptions.

**Witori** — The Witori caldera has produced three VEI 6 eruptions in ~5,000 years (~4000 BCE, ~1370 BCE, 710 CE) — an exceptional rate of catastrophic activity. The active Pago cone within the caldera last erupted in 2012.

**Billy Mitchell** — This Bougainville caldera produced a VEI 6 eruption around 1580 CE. Quiet since then, it represents a potentially dangerous ‘sleeping giant.’

**Kadovar** — This small volcanic island erupted dramatically in 2018 after centuries of dormancy, forcing evacuation of its ~600 residents. Activity continued through 2023.

Eruption History

Papua New Guinea’s volcanic eruption history is one of the most violent in the Pacific, with 261 confirmed eruptions across 39 volcanoes. The country has produced 8 VEI 6 eruptions during the Holocene — rivaling [[country:indonesia|Indonesia]] — alongside 4 VEI 5, 19 VEI 4, and 36 VEI 3 events. The VEI distribution is dominated by moderate explosive eruptions (127 events at VEI 2, 49% of eruptions with assigned VEI).

The largest Holocene eruptions include Witori’s three VEI 6 events (~4000 BCE, ~1370 BCE, 710 CE), Dakataua (~653 CE, VEI 6), Rabaul (~683 CE, VEI 6), Long Island (~2040 BCE and ~1660 CE, both VEI 6), and Billy Mitchell (~1580 CE, VEI 6). These collectively demonstrate that PNG’s arcs produce Krakatoa-scale explosions with alarming regularity.

The historical period saw devastating activity: the 1937 Rabaul eruption killed 507 people; the 1951 Lamington disaster killed 2,942; the 1994 Rabaul eruption buried the city. The 21st century has maintained PNG’s high eruption tempo: Manam’s 2004 VEI 4 eruption displaced the entire island population; Ulawun erupted explosively in 2019 with a 19-km column; Kadovar’s unexpected 2018 eruption evacuated its island. As of 2025, four PNG volcanoes are simultaneously active: Ulawun, Bagana, Manam, and Langila.

Volcanic Hazards

Papua New Guinea faces a comprehensive spectrum of volcanic hazards compounded by challenging island geography, limited infrastructure, and isolated communities. Pyroclastic flows represent the greatest lethal threat, as demonstrated by the 1951 Lamington disaster (2,942 deaths). The steep-sided andesitic stratovolcanoes of the Bismarck arc are all capable of generating devastating pyroclastic flows.

Tephra fall persistently affects agriculture and infrastructure. The 1994 Rabaul eruption deposited meters of wet ash that collapsed buildings. Volcanic tsunamis pose particular danger in PNG’s island setting — the ~1660 CE Long Island eruption generated a tsunami, and the 1888 Ritter Island collapse produced a massive debris avalanche and tsunami.

Volcanic gas emissions affect communities downwind of persistently degassing volcanoes.

The Rabaul Volcanological Observatory (RVO) monitors PNG’s volcanoes using seismometers, tiltmeters, and visual observations, supplemented by satellite monitoring from international partners including the Australian Bureau of Meteorology, [[ext:https://www.usgs.gov/programs/volcano-hazards|USGS]], and Japan Meteorological Agency. PNG’s total population at volcanic risk is estimated at several hundred thousand.

Volcanic Zones Map

PNG’s volcanoes span four provinces. The Bismarck Volcanic Arc along New Britain’s north coast is the most active zone, hosting Ulawun, Rabaul, Langila, Witori, Bamus, Karkar, and Dakataua. The Bougainville Volcanic Arc hosts Bagana, Balbi (PNG’s tallest at 2,715 m), Billy Mitchell, and Loloru.

The Trobriand Volcanic Province on the Papuan mainland includes Lamington, Victory, and Dawson Strait Group. The Bismarck Sea Volcanic Province includes submarine and near-sea-level features. Manam, Karkar, Long Island, Bam, and Kadovar form a chain extending north from the mainland into the Bismarck Sea.

Impact On Culture And Economy

Volcanoes have profoundly shaped Papua New Guinea’s diverse indigenous communities. The Tolai people of Rabaul have coexisted with the caldera for millennia, and their oral traditions include eruption accounts. The 1994 eruption displaced the entire community and shifted the provincial capital to Kokopo.

On Manam Island, ~9,000 residents evacuated in 2004 remain largely displaced — one of the Pacific’s longest-running volcanic displacement crises. Volcanic soils support productive agriculture, particularly cocoa and copra in the Gazelle Peninsula. PNG’s volcanic landscapes are increasingly recognized for tourism potential, though infrastructure remains limited.

Visiting Volcanoes

Volcanic tourism in Papua New Guinea requires adventurous preparation and tolerance for basic infrastructure. Rabaul on New Britain, accessible by air from Port Moresby, offers the most developed experiences: the buried old town, Tavurvur cone viewpoints, the volcanological observatory, and hot springs. The Rabaul area includes World War II sites from the Japanese occupation.

More remote volcanoes require charter flights or boats. Visitors should check alert levels with the Rabaul Volcanological Observatory, travel with local guides, and prepare for unpredictable logistics. The dry season (May–October) offers the best conditions.

Volcanoes

Volcano Table

Rank Name Elevation (m) Type Last Eruption EvidenceEruptions VEI Max
1Balbi2,715StratovolcanoUnknownHolocene0VEI —
2Ulawun2,334Stratovolcano2025Active47VEI 4
3Bamus2,248Stratovolcano1886Active4VEI 3
4Takuan Group2,210CompoundUnknownHolocene0VEI —
5Hydrographers Range1,915StratovolcanoUnknownHolocene0VEI —
6Loloru1,887Compound1050 BCEActive6VEI —
7Bagana1,855Lava cone2025Active25VEI 4
8Karkar1,839Stratovolcano1979Active11VEI 4
9Victory1,832Stratovolcano1935Active1VEI 2
10Manam1,807Stratovolcano2025Active41VEI 4
11Lamington1,680Stratovolcano1956Active3VEI 4
12Billy Mitchell1,544Caldera1580Active2VEI 6
13Managlase Plateau1,342Volcanic fieldUnknownHolocene0VEI —
14Umboi1,335ComplexUnknownHolocene0VEI —
15Langila1,330Complex2025Active26VEI 3
16Long Island1,263Complex1993Active11VEI 6
17Hargy1,148Stratovolcano950Active2VEI —
18Bola1,116StratovolcanoUnknownHolocene0VEI —
19Sakar947StratovolcanoUnknownHolocene0VEI —
20Lolobau878Caldera1912Active3VEI 4
21Lolo796StratovolcanoUnknownHolocene0VEI —
22Witori724Caldera2012Active19VEI 6
23Rabaul688Caldera2014Active19VEI 6
24Bam685Stratovolcano1960Active17VEI 3
25Sulu Range610Stratovolcano(es)UnknownHolocene0VEI —
26Garua Harbour565Volcanic fieldUnknownHolocene0VEI —
27Krummel-Garbuna-Welcker564Stratovolcano(es)2008Active4VEI 2
28Dawson Strait Group500Volcanic field1350Active1VEI —
29Sessagara Hills493Volcanic field1944Active1VEI 3
30Dakataua408Caldera1895Active3VEI 6
31Blup Blup402StratovolcanoUnknownHolocene0VEI —
32Kadovar365Stratovolcano2023Active1VEI 2
33St. Andrew Strait270Complex1957Active4VEI 2
34Goodenough220Volcanic fieldUnknownHolocene0VEI —
35Tavui200Caldera4946 BCEActive1VEI 5
36Iamalele194Lava dome(s)UnknownHolocene0VEI —
37Ritter Island75Stratovolcano2007Active8VEI 3
38Hankow Reef-5StratovolcanoUnknownHolocene0VEI —
39Central Bismarck Sea-1,300Fissure vent1972Active1VEI 0
Showing 39 of 39 volcanoes

Interesting Facts

  1. 1Papua New Guinea has 39 Holocene volcanoes but 261 confirmed eruptions — an average of nearly 7 per volcano, one of the highest ratios on Earth.
  2. 2PNG has produced 8 VEI 6 eruptions during the Holocene, events comparable to 1883 Krakatoa, more than almost any other country.
  3. 3The 1951 Lamington eruption killed 2,942 people — one of the deadliest volcanic disasters of the 20th century, worsened because Lamington was not recognized as active.
  4. 4Witori caldera has produced three VEI 6 eruptions in ~5,000 years — an exceptional rate of catastrophic activity for a single volcanic center.
  5. 5The 1994 Rabaul eruption buried the former largest town on New Britain under meters of ash, permanently relocating the provincial capital to Kokopo.
  6. 6Four PNG volcanoes are simultaneously active in 2025 (Ulawun, Bagana, Manam, Langila), highlighting extraordinary eruption frequency.
  7. 7Manam Island’s ~9,000 residents evacuated in 2004 remain largely displaced over two decades later — one of the Pacific’s longest volcanic displacement crises.
  8. 8Bagana may have built its entire 1,855-m edifice in just 300 years through persistent lava extrusion — one of the fastest-growing volcanoes on Earth.
  9. 9Ulawun, called ‘The Father’ by locals, is a designated Decade Volcano due to its explosive potential near populated areas.
  10. 10The 1888 Ritter Island collapse generated one of the largest historically documented volcanic tsunamis in the Pacific.
  11. 11PNG’s Central Bismarck Sea volcano at -1,300 m is the deepest confirmed eruption site in the southwestern Pacific.
  12. 12Billy Mitchell caldera has been quiet since its ~1580 CE VEI 6 eruption but its proven catastrophic capacity makes it a dangerous sleeping giant.

Frequently Asked Questions

How many volcanoes are in Papua New Guinea?

Papua New Guinea has 39 Holocene volcanoes listed in the Smithsonian Global Volcanism Program database, making it the seventh most volcanically active country on Earth. These volcanoes are distributed across the islands of New Britain (the most volcanically dense), Bougainville, the Bismarck Sea islands, and the Papuan mainland. The count includes stratovolcanoes, calderas, complex volcanoes, volcanic fields, lava cones, and one submarine fissure vent. Despite having fewer total volcanoes than some countries, PNG's high eruption frequency (261 confirmed events) makes it one of the most volcanically dynamic nations on the planet.

What is Papua New Guinea's most active volcano?

Ulawun, with 47 confirmed eruptions, is PNG's most active volcano by eruption count. Known as 'The Father' by local communities, this 2,334-m stratovolcano on New Britain has erupted repeatedly throughout historical records and was active in 2025. Manam ranks second (41 eruptions), followed by Langila (26 eruptions), Bagana (25 eruptions), and Rabaul and Witori (19 each). In terms of continuous activity, Bagana has been in near-constant eruption since 1972, producing persistent lava extrusion and Vulcanian explosions.

What is the most dangerous volcano in Papua New Guinea?

Manam and Rabaul are widely considered PNG's most dangerous volcanoes. Manam's combination of VEI 4 explosive capability, channeled pyroclastic flows down four radial valleys, and a population living at the volcano's base has resulted in repeated devastation and displacement. Rabaul caldera's proven capacity for VEI 6 eruptions and its location adjacent to populated areas makes it a persistent long-term threat. Ulawun is designated a Decade Volcano due to its explosive potential and proximity to communities. Lamington demonstrated that even unrecognized volcanoes can produce devastating eruptions without warning.

What happened in the 1994 Rabaul eruption?

On September 19, 1994, Rabaul caldera on New Britain erupted simultaneously from two vents: Vulcan and Tavurvur. The dual eruption produced massive ash columns, pyroclastic flows, and heavy tephra fall that buried much of the city of Rabaul under meters of wet ash, collapsing buildings and destroying infrastructure. Approximately 17,000 people were evacuated. Remarkably, only 5 people died, largely because years of seismic monitoring and public education enabled a rapid evacuation when precursory earthquakes intensified. The provincial capital was permanently relocated to Kokopo, 20 km southeast.

What was the Lamington disaster?

The 1951 eruption of Mount Lamington on January 21 was one of the deadliest volcanic disasters of the 20th century. The catastrophic VEI 4 Plinian eruption generated pyroclastic flows that devastated an area of 230 square kilometers on the Papuan Peninsula, killing approximately 2,942 people. The disaster was especially tragic because Lamington was not recognized as an active volcano before the eruption, so no monitoring or evacuation plans existed. The event led to the establishment of the Rabaul Volcanological Observatory and fundamentally changed volcanic monitoring in PNG.

Is Papua New Guinea on the Ring of Fire?

Yes, Papua New Guinea sits squarely on the Ring of Fire, the horseshoe-shaped zone of intense volcanic and seismic activity encircling the Pacific Ocean. PNG occupies one of the most tectonically complex sections of the Ring, where multiple microplates (Pacific, Solomon Sea, South Bismarck, North Bismarck) converge with the Indo-Australian Plate. This creates multiple overlapping subduction zones and volcanic arcs. About 75% of the world's active volcanoes are on the Ring of Fire, and PNG's 39 volcanoes and 261 confirmed eruptions make it one of the Ring's most active segments.

Can you visit volcanoes in Papua New Guinea?

Volcanic tourism in Papua New Guinea is possible but requires adventurous preparation and tolerance for basic infrastructure. Rabaul on New Britain offers the most accessible volcanic experiences, including views of Tavurvur cone, the buried old town, and hot springs. Flights connect Rabaul (Tokua airport) to Port Moresby and Lae. For more remote volcanoes, charter flights or boat transport are necessary. Visitors should always check alert levels with the Rabaul Volcanological Observatory, travel with experienced local guides, and be prepared for unpredictable weather and logistics. The dry season (May-October) offers the best conditions.

How many VEI 6 eruptions has PNG had?

Papua New Guinea has experienced 8 VEI 6 eruptions during the Holocene, an extraordinary count that rivals Indonesia for the most cataclysmic volcanic activity in the Pacific. These events occurred at Witori (three times: ~4000 BCE, ~1370 BCE, and 710 CE), Rabaul (~683 CE), Dakataua (~653 CE), Long Island (twice: ~2040 BCE and ~1660 CE), and Billy Mitchell (~1580 CE). VEI 6 eruptions are comparable in scale to the 1883 Krakatoa eruption and are capable of devastating entire islands, generating tsunamis, and affecting regional climate.

Why are PNG's volcanoes so explosive?

PNG's volcanoes are highly explosive primarily because of the andesitic to dacitic magma compositions produced by the subduction zones beneath the island arcs. These intermediate-composition magmas contain higher volatile contents (water, CO2, sulfur) than basaltic magmas, and their higher viscosity traps gas bubbles until pressure builds to explosive levels. The relatively thin oceanic crust beneath PNG's arcs allows magma to stall at shallow depths where volatile exsolution drives explosive fragmentation. Additionally, the high convergence rates (7-10 cm/year) drive rapid magma production, feeding frequent eruptions.