🌋VolcanoAtlas

Sete Cidades

The Twin-Lake Caldera of the Azores

Elevation

842 m

Last Eruption

1880

Type

Stratovolcano

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 RiskModerate
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 Activity146 years agoHistoricalHistorically active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Normal
No recent activity. Routine monitoring continues.
green grass field and mountain under blue sky during daytime

Rui Amaro

via Unsplash

an aerial view of a large building in the middle of a forest

Kalyan Mukherjee

via Unsplash

a body of water surrounded by trees

António Cunha

via Unsplash

Other Volcanoes in Portugal

Interesting Facts

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Sete Cidades' caldera formed approximately 22,000 years ago in a catastrophic collapse, creating a 5-km-wide depression that is one of the largest calderas in the Azores.

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The twin caldera lakes — Lagoa Azul (Blue Lake) and Lagoa Verde (Green Lake) — were voted one of the Seven Natural Wonders of Portugal in 2010.

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At least 22 post-caldera eruptions have occurred at Sete Cidades, with a nearly circular ring of six Holocene pyroclastic cones on the caldera floor marking the most recent vents.

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The 1444 eruption was the last VEI 4 event at Sete Cidades and occurred less than a decade after Portuguese settlement of São Miguel, disrupting the fledgling colony.

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Four of the last five eruptions at Sete Cidades originated from submarine vents off the western coast, indicating that the volcano's magmatic plumbing extends well offshore.

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The volcano's trachytic magma composition makes its eruptions significantly more explosive than basaltic eruptions typical of mid-ocean ridges.

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Sete Cidades sits at the Azores Triple Junction where three tectonic plates — Eurasian, Nubian, and North American — interact, one of only a handful of triple junctions on Earth.

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The village of Sete Cidades (population ~800) sits on the caldera floor, making it one of the few inhabited volcanic calderas in Europe.

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The 1811 submarine eruptions produced two separate events in the same year, generating floating pumice rafts that disrupted Atlantic shipping lanes.

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Ferraria, a geothermally heated ocean swimming area on the volcano's southwest coast, reaches temperatures of up to 40°C where volcanic hot springs meet the Atlantic.

Frequently Asked Questions

Is Sete Cidades an active volcano?
Yes, Sete Cidades is classified as an active volcano by the Smithsonian Global Volcanism Program. It last erupted in 1880 from a submarine vent off the western coast of São Miguel Island in the Azores. The volcano has produced 16 documented eruptions over the past 5,000 years, with an average recurrence interval of roughly 300 years. CIVISA, the Azores' volcanological monitoring center, continuously tracks seismicity and gas emissions from the caldera. Scientists consider a future eruption virtually certain on geological timescales, though the timing remains unpredictable.
Why are the lakes at Sete Cidades different colors?
The two main caldera lakes — Lagoa Azul (Blue Lake) and Lagoa Verde (Green Lake) — appear to have different colors primarily due to differences in depth, light reflection, and algal content. Lagoa Azul is deeper and reflects the sky's blue tones more prominently, while the shallower Lagoa Verde supports more algal growth, lending it a greenish hue. The effect is most pronounced on clear, sunny days. Local legend attributes the colors to the tears of a princess (blue) and a shepherd (green) whose forbidden love created the lakes.
When did Sete Cidades last erupt?
The most recent eruption at Sete Cidades occurred in 1880, from a submarine vent off the western coast of São Miguel Island. This was a relatively minor event (VEI 0). The last on-land eruption took place in 1713 at Pico das Camarinhas on the western flank (VEI 2). The last major explosive eruption from the caldera itself was in 1444, a VEI 4 event at Caldeira Seca that produced significant trachytic pumice fall deposits across western São Miguel.
Can you visit Sete Cidades caldera?
Yes, Sete Cidades is the most popular natural attraction in the Azores and is easily accessible from Ponta Delgada, the island's capital, about 15 km to the east (a 30-minute drive). The classic viewpoint is Miradouro da Vista do Rei on the southern caldera rim. Visitors can hike rim trails, descend to the lakeshores, kayak on Lagoa Azul, and explore the village of Sete Cidades on the caldera floor. The geothermally heated ocean pools at Ferraria are also nearby. Entry to the caldera area is free.
How dangerous is Sete Cidades?
Sete Cidades poses a moderate volcanic hazard. Its trachytic magma composition favors explosive eruptions, and its caldera has produced four VEI 4 events in the past 5,000 years. Approximately 13,000 people live in the surrounding parishes, and the village of Sete Cidades sits on the caldera floor. A major eruption could produce pyroclastic flows, heavy pumice fall, and lahars. Ponta Delgada (population ~68,000), 15 km east, could experience significant ashfall. CIVISA and the Azores civil protection authority maintain evacuation plans.
What type of volcano is Sete Cidades?
Sete Cidades is classified as a stratovolcano with a summit caldera. Stratovolcanoes are composite volcanoes built from alternating layers of lava and pyroclastic material. Its defining feature is the 5-km-wide caldera, formed by a catastrophic collapse approximately 22,000 years ago. Post-caldera activity has built pyroclastic cones, lava domes, and cinder cones both within and outside the caldera. Its trachytic magma — more silica-rich than typical oceanic basalt — produces moderately to highly explosive eruptions.
How many volcanoes are on São Miguel Island?
São Miguel Island hosts three major active polygenetic volcanic centers: Sete Cidades at the western end, Agua de Pau (with Lagoa do Fogo) in the center, and Furnas at the eastern end. Additionally, the Picos Volcanic Fissure Zone lies between Sete Cidades and Agua de Pau, and the Nordeste shield volcano (now dormant) forms the island's eastern tip. In total, São Miguel contains five distinct volcanic systems, making it one of the most volcanically complex islands in the Atlantic.