🌋VolcanoAtlas

Terceira

The Azores' Multi-Volcano Island on the Mid-Atlantic Rift

Elevation

1,023 m

Last Eruption

1998–2000 (submarine)

Type

Stratovolcano(es)

Country

Portugal

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 Activity-19979974 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 Portugal

Interesting Facts

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Terceira's 1998–2000 submarine eruption produced rare 'lava balloons' — hollow basaltic spheres up to 1 m in diameter that floated to the ocean surface.

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The island contains four distinct volcanic centers — Santa Bárbara, Pico Alto, Guilherme Moniz, and Cinco Picos — each with its own caldera or summit structure.

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Angra do Heroísmo, on Terceira's southern coast, is a UNESCO World Heritage Site and was a crucial port for Portuguese maritime exploration and Atlantic trade.

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A magnitude 7.2 earthquake struck near Terceira in 1980, killing 61 people and causing severe damage to Angra do Heroísmo's historic center.

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Terceira's volcanic system extends well beyond the island's coastline, with the submarine Serreta Ridge representing an active volcanic segment to the west.

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The island's name means 'third' in Portuguese, referring to its order of discovery during the colonization of the Azores in the 15th century.

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Algar do Carvão, a volcanic chimney and lava tube on Terceira, descends about 90 m into the Earth and features a subterranean lake with rare silica stalactites.

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Terceira sits near the Azores Triple Junction where three tectonic plates — North American, Eurasian, and African — interact, making it one of the most tectonically complex volcanic settings in the Atlantic.

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The Cinco Picos caldera at Terceira's southeastern end is 7 km in diameter — the largest caldera structure on the island.

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Approximately 56,000 people live on Terceira, making it one of the most densely populated volcanic islands in the mid-Atlantic.

Frequently Asked Questions

Is Terceira volcano active?
Yes, Terceira is an active volcanic island. Its most recent eruption was a submarine event along the Serreta Ridge from 1998 to 2000. The most recent on-land eruption occurred in 1761 along the island's central fissure zone. With 15 recorded eruptions over nearly 9,000 years and its position on the tectonically active Azores Triple Junction, Terceira is considered fully capable of future eruptions. CIVISA, the Azores' seismic and volcanic monitoring center, maintains continuous surveillance of the island's volcanic systems.
When did Terceira last erupt?
Terceira's most recent eruption occurred from November 25, 1998, to 2000, when a submarine vent on the Serreta Ridge west of the island produced low-intensity lava effusion. The eruption generated distinctive lava balloons that floated to the ocean surface. The most recent eruption on the island itself was in 1761, when a fissure eruption east of Santa Bárbara volcano produced basaltic lava flows. A more powerful submarine eruption (VEI 3) occurred in 1867 approximately 3–6 km west-northwest of the island.
What are the main volcanic attractions on Terceira?
Terceira offers several volcanic attractions. Algar do Carvão is a spectacular volcanic chimney and lava tube descending about 90 m underground, featuring a subterranean lake and rare silica stalactites — it is one of the most visited volcanic caves in the Azores. Furnas do Enxofre is an active fumarole field and hot springs area on the slopes of Santa Bárbara volcano. The Santa Bárbara caldera trail provides panoramic views. The island's calderas, cinder cones, and lava landscapes are accessible via well-marked hiking trails. Angra do Heroísmo adds cultural depth with its UNESCO-listed historic center.
How many volcanoes are on Terceira?
Terceira contains four distinct volcanic centers: Santa Bárbara (the youngest and highest at 1,023 m), Pico Alto, Guilherme Moniz, and Cinco Picos. These are connected by a prominent ESE-WNW fissure zone that has also been the source of independent eruptions. Additionally, the submarine Serreta Ridge extends the volcanic system west of the island. Rather than a single volcano, Terceira is best understood as a multi-center volcanic island where eruptions can occur from several different vents and fissures.
Is Terceira at risk of earthquakes?
Yes, Terceira faces significant seismic risk in addition to volcanic hazards. The island sits at the intersection of major tectonic plate boundaries. A magnitude 7.2 earthquake struck near Terceira on January 1, 1980, killing 61 people and causing extensive damage in Angra do Heroísmo and surrounding communities. The earthquake triggered a major reconstruction effort that ultimately contributed to the city's UNESCO designation. Smaller earthquakes occur regularly across the Azores, and CIVISA monitors seismic activity continuously.
What are lava balloons?
Lava balloons are hollow, gas-filled spheres of basaltic lava produced during submarine volcanic eruptions. During Terceira's 1998–2000 Serreta Ridge eruption, lava balloons up to 1 m in diameter floated to the ocean surface, where they were collected by scientists and fishermen. They form when molten lava in contact with seawater develops a rapidly cooled outer shell while volcanic gases trapped inside create buoyancy. Once the gas leaks out, the balloons eventually sink. These formations are rare and scientifically valuable as direct samples from active submarine eruptions.