πŸŒ‹VolcanoAtlas

Hunga Tonga-Hunga Ha'apai

The Eruption That Shook the World

Elevation

114 m

Last Eruption

2022

Type

Caldera

Country

Tonga

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows and surges
  • Large explosive eruptions (VEI 4+)
  • Ash fall and tephra deposits
  • Lahars and debris flows

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 Activity4 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 Tonga

Interesting Facts

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The January 15, 2022 eruption produced the highest volcanic plume ever measured by satellite β€” approximately 57 km (187,000 ft), reaching the mesosphere.

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The atmospheric shockwave from the eruption circled the globe at least six times and was detected by barometers on every continent.

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The sonic boom was reportedly audible in New Zealand, 2,000 km away, and possibly as far as Alaska, over 9,000 km distant.

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The eruption injected approximately 146 teragrams (146 million metric tons) of water vapor into the stratosphere β€” increasing global stratospheric moisture by roughly 10%.

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The tsunami generated by the eruption killed people in Peru, more than 10,000 km from the source.

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The eruption severed Tonga's single undersea fiber-optic communications cable, leaving the island nation without international communications for over a month.

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The 2014–2015 eruption created one of the few new volcanic islands formed in the 21st century, studied by NASA as an analog for volcanic processes on Mars.

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Geological research revealed at least three previous caldera-forming eruptions in the volcano's history, suggesting a cycle of catastrophic collapse and rebuilding.

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The 2022 eruption is widely compared to the 1883 eruption of Krakatoa in terms of explosive violence, atmospheric effects, and tsunami generation.

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Unlike most large eruptions that cool the climate via sulfate aerosols, the Hunga Tonga eruption's massive water vapor injection may have produced a slight warming effect.

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Wave heights of 15–20 m were recorded on some islands near the volcano during the 2022 tsunami.

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The eruption destroyed most of the combined island that had formed during the 2014–2015 eruption, leaving only small remnants above sea level.

Frequently Asked Questions

How powerful was the 2022 Hunga Tonga eruption?
The January 15, 2022 eruption of Hunga Tonga-Hunga Ha'apai was one of the most powerful volcanic explosions in recorded history, rated at least VEI 5. The eruption plume reached approximately 57 km altitude β€” the highest ever measured by satellite β€” penetrating the mesosphere. It generated atmospheric shockwaves that circled the globe multiple times, a Pacific-wide tsunami, and injected 146 teragrams of water vapor into the stratosphere. The explosion has been widely compared to the 1883 eruption of Krakatoa.
How many people died in the Hunga Tonga eruption?
The 2022 eruption caused at least 6 deaths β€” 4 in Tonga from the tsunami and volcanic effects, and 2 in Peru from tsunami waves that traveled over 10,000 km across the Pacific. Given the eruption's extreme violence, the relatively low death toll reflects the volcano's remote submarine location, 65 km from Tongatapu. However, the eruption caused extensive damage to Tongan infrastructure, agriculture, and communications, affecting the entire nation of approximately 100,000 people.
Did the Hunga Tonga eruption affect global climate?
The eruption injected approximately 146 teragrams of water vapor into the stratosphere, increasing global stratospheric moisture by roughly 10% β€” an unprecedented event. Unlike sulfate aerosol injections from eruptions like Pinatubo (1991), which cool the planet, stratospheric water vapor acts as a greenhouse gas and may produce slight warming. Research suggests this water vapor could persist for 5–10 years. The eruption also injected sulfur dioxide, but in smaller quantities than the largest climate-altering eruptions.
Where is Hunga Tonga-Hunga Ha'apai located?
Hunga Tonga-Hunga Ha'apai is a submarine caldera volcano in the Kingdom of Tonga, at approximately 20.55Β°S, 175.38Β°W in the southwestern Pacific Ocean, about 65 km north of Tongatapu, Tonga's main island. It lies along the Tofua Volcanic Arc, formed by the subduction of the Pacific Plate beneath the Indo-Australian Plate. The caldera is approximately 6 km in diameter, with most of its rim below sea level.
Could Hunga Tonga erupt again?
Yes. Geological evidence reveals at least three previous caldera-forming eruptions in the volcano's history, including a major event dated to approximately 1040–1180 CE. This indicates a pattern of repeated large-scale eruptions. While another eruption of the 2022 scale is unlikely in the near term β€” the volcano likely exhausted a significant portion of its immediately available magma β€” future submarine eruptions and island-building events are considered probable on geological timescales.
What happened to the islands after the 2022 eruption?
The January 15, 2022 explosion destroyed most of the combined island that had formed when the 2014–2015 eruption connected Hunga Tonga and Hunga Ha'apai. Only small, low-lying remnants of the original caldera rim remain above sea level. Bathymetric surveys showed the caldera floor was significantly deepened. The 2014–2015 island β€” which had been studied as a natural laboratory for ecological succession β€” was almost entirely obliterated.