🌋VolcanoAtlas

Home Reef

The Island-Making Submarine Volcano of Tonga

Elevation

-10 m

Last Eruption

2025

Type

Submarine Stratovolcano

Country

Tonga

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 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.
an island in the middle of the ocean

Pascal Müller

via Unsplash

A small island in the middle of a body of water

Salvatore Tonnara

via Unsplash

an island in the middle of a body of water

Pascal Scholl

via Unsplash

brown mountain near body of water during daytime

Peace Itimi

via Unsplash

Volcanic island in the ocean with rocky shoreline

Krzysztof

via Unsplash

white clouds over snow covered mountain

Marek Piwnicki

via Unsplash

Other Volcanoes in Tonga

Interesting Facts

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Home Reef has built and lost at least four ephemeral volcanic islands since 1852, each emerging from the ocean during eruptions and eroding away within weeks to months.

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The 1984 eruption produced a temporary island with cliffs reaching 30–50 m above sea level — taller than a 10-story building — enclosing a water-filled crater.

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Pumice rafts from the 2006 eruption drifted over 3,000 km across the Pacific Ocean, eventually washing up on Australian beaches.

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Home Reef's dacitic magma composition is unusually silica-rich for an oceanic volcanic arc, contributing to its explosive, island-building eruption style.

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The Tonga Trench, located 150 km east of Home Reef, plunges to over 10,800 m — making the region home to both the deepest ocean trench and some of the most active submarine volcanoes on Earth.

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Six of Home Reef's nine recorded eruptions have occurred in the 21st century (since 2006), indicating a substantial increase in activity.

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Home Reef lies approximately 400 km north of Hunga Tonga-Hunga Ha'apai, whose January 2022 eruption was one of the most powerful volcanic explosions in recorded history.

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Scientists have tracked pumice rafts from Home Reef via satellite to study how floating volcanic rock transports marine organisms between remote island ecosystems.

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The Tonga-Kermadec subduction zone converges at approximately 24 cm/year — the fastest plate convergence rate on Earth — fueling the arc's prolific volcanic activity.

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Home Reef's summit depth fluctuates with each eruption-erosion cycle; during quiescence it sits approximately 10 m below sea level, but it can emerge as high as 50 m above during major eruptions.

Frequently Asked Questions

Is Home Reef still active?
Yes, Home Reef is one of the most active submarine volcanoes on Earth. It has been erupting intermittently since 2022, with confirmed activity in 2022, 2023, 2024 (twice), and 2025. The volcano has produced nine documented eruptions since 1852. It is monitored via satellite by agencies including NASA and the Tonga Geological Service. The current period of heightened activity suggests an ongoing magma supply, and further eruptions are expected.
Does Home Reef create islands?
Yes, Home Reef is famous for repeatedly building volcanic islands that rise above the ocean surface during eruptions, then erode away within weeks to months. At least four ephemeral islands have been documented: in 1852, 1984, 2006, and 2022. The 1984 island was the largest, measuring 500 × 1,500 m with cliffs up to 50 m high. These islands form from accumulated pumice and ash, which lack the structural cohesion to resist Pacific wave erosion, so they invariably disappear.
What are pumice rafts?
Pumice rafts are floating masses of volcanic pumice rock that form when explosive eruptions fragment magma into highly porous, gas-filled rock that is less dense than water. During eruptions, Home Reef produces enormous volumes of dacitic pumice that float on the ocean surface, forming rafts that can cover thousands of square kilometers. These rafts drift with ocean currents for months, sometimes crossing entire ocean basins — the 2006 Home Reef pumice raft traveled over 3,000 km to reach Australia.
Is Home Reef dangerous?
Home Reef poses low direct risk to human populations since no islands are inhabited nearby (the closest is Late Island, 55 km south). However, its eruptions create maritime hazards: pumice rafts can damage ship engines, ephemeral islands and shoaling create uncharted shallow waters, and volcanic ash can affect aviation. Submarine eruptions carry a small risk of generating local tsunami waves. The volcano is far less dangerous than its neighbor Hunga Tonga-Hunga Ha'apai, which produced a devastating eruption in 2022.
Where is Home Reef located?
Home Reef is located at approximately 18.99°S, 174.78°W in the central Tonga Islands, South Pacific Ocean. It sits within the Tofua Volcanic Arc, part of the broader Tonga-Kermadec subduction zone, midway between Metis Shoal to the north and Late Island to the south. The Kingdom of Tonga's capital, Nuku'alofa, lies approximately 350 km to the south-southwest. The volcano is situated about 150 km west of the Tonga Trench.
How deep is Home Reef?
Home Reef's summit depth varies with eruption cycles. During quiescent periods, the summit sits approximately 10 m (33 ft) below sea level. During eruptions, the summit can emerge above sea level by tens of meters — the 1984 island had cliffs up to 50 m high. After eruptions cease, wave erosion reduces the island back below the surface. The surrounding seafloor drops off rapidly to depths exceeding 1,000 m within a few kilometers of the volcano.