Last updated August 27, 2025

The Largest Calderas in the World: Earth's Scars

Volcanic calderas: Earth's giant scars

A caldera (from the Portuguese "caldeira," meaning "cauldron") is a vast volcanic depression, usually circular, formed by the collapse of the roof of a magma chamber emptied after a major volcanic eruption. Unlike explosion craters, which are smaller and formed by explosive eruptions, calderas measure tens of kilometers in diameter and bear witness to cataclysmic events that have shaped the geological history of our planet.

Formation mechanisms

The formation of a caldera follows a complex geological process. During a super-eruption, enormous volumes of magma (generally > 1000 km³) are expelled in a relatively short time. The partially emptied magma chamber can no longer support the weight of the overlying rocks, causing the structure to collapse and create a depression. There are mainly three types of calderas:

Collapse calderas (the most common)
Explosion calderas (rarer)
Erosion calderas (formed by the erosion of volcanoes)

The most impressive calderas on the planet

Our planet is home to several monumental calderas, witnesses to cataclysmic events that have shaped landscapes and influenced Earth's climate.

Table of characteristics of the world's main calderas
Name	Location	Diameter (km)	Ejected volume (km³)	Age of formation	Type of caldera
La Garita	Colorado, USA	35 × 75	> 5000	27.8 million years	Collapse (ignimbrite)
Toba	Sumatra, Indonesia	100 × 30	2800	74,000 years	Collapse (supervolcano)
Yellowstone	Wyoming, USA	85 × 45	1000	640,000 years	Collapse (hotspot)
Taupo	North Island, New Zealand	35	1200	26,500 years	Collapse (volcanic arc)
Long Valley	California, USA	32 × 17	600	760,000 years	Collapse (volcanic complex)
Valle Grande	New Mexico, USA	22	300	1.25 million years	Collapse (ignimbrite)
Aira	Kyushu, Japan	20	400	22,000 years	Collapse (subduction)
Campi Flegrei	Naples, Italy	13	500	39,000 years	Collapse (complex volcanic zone)
Santorini	Greece	11	60	1600 BCE	Collapse (Aegean arc)
Krakatoa	Indonesia	7	25	1883	Collapse (volcanic arc)
Ngorongoro	Tanzania	20	150	2.5 million years	Collapse (continental rift)
Cerro Galán	Argentina	34	1000	2.2 million years	Collapse (ignimbrite)
Kilauea	Hawaii, USA	4 × 3.2	20	Continuously forming	Collapse (hotspot)
Crater Lake	Oregon, USA	8 × 10	50	7,700 years	Collapse (composite volcano)
Askja	Iceland	8	45	1875	Collapse (Mid-Atlantic Rift)
Rabaul	Papua New Guinea	14	100	1,400 years	Collapse (volcanic arc)
Okataina	New Zealand	26	350	64,000 years	Collapse (volcanic arc)
Valles	New Mexico, USA	22	400	1.25 million years	Collapse (ignimbrite)
Ijen	Java, Indonesia	1	5	50,000 years	Explosion (acidic)
Aniakchak	Alaska, USA	10	50	3,400 years	Collapse (Aleutian arc)

Source: Smithsonian Institution - Global Volcanism Program and United States Geological Survey.

Impact on climate and environment

Super-eruptions forming calderas have catastrophic consequences on a planetary scale. The injection of large amounts of ash and sulfur aerosols into the stratosphere can cause a "volcanic winter" with a significant drop in global temperatures for several years. The Toba eruption, 74,000 years ago, may have caused a global cooling of 3 to 5°C and a bottleneck in the human population, possibly reducing our species to just a few thousand individuals.

N.B.: A volcanic winter is a temporary drop in global temperatures caused by large volcanic eruptions. Ash and sulfur gases projected into the stratosphere reflect solar light, reducing the energy received at the surface.

The Blue Caldera: Oregon's Mirror of the Sky

Monitoring and current risks

The large calderas on our planet are visible scars of cataclysmic events that have marked Earth's history. Studying them informs us not only about extreme geological processes but also about the fragility of our civilization in the face of natural forces. Understanding these colossal volcanic systems is essential for assessing future risks and developing mitigation strategies for eruptions that, although rare, could one day recur.

Several large calderas, such as Yellowstone, Campi Flegrei (Italy), or Aira (Japan), still host active magmatic systems. They are closely monitored by volcanologists who measure ground deformation, seismic activity, gas emissions, and thermal variations. Although the risk of a super-eruption in the short term is statistically low, its consequences would be so dramatic that the international scientific community is closely watching these "sleeping giants".