By VolcanoDB Research Team. Data: Smithsonian Global Volcanism Program, 11,079 eruptions.
How We Rank Eruptions — VEI and Volume
I've ranked these eruptions by total volume of material ejected — not by death toll, not by cultural impact, and not by how often they show up in clickbait articles. Volume is the most objective measure of raw volcanic power, and it's directly tied to the Volcanic Explosivity Index (VEI), the logarithmic scale volcanologists use to classify eruptions.
Each VEI step represents a tenfold increase in ejected material. A VEI 5 eruption like Mount St. Helens (1980) produced about 1 km³. A VEI 6 like Pinatubo: 10 km³. A VEI 7 like Tambora: 100+ km³. And a VEI 8 — the so-called super-eruptions — start at 1,000 km³ and go far higher.
Our database tracks 11,079 eruptions from the Smithsonian's Global Volcanism Program. Of those, 240 are rated VEI 5 or higher, and 7 are confirmed VEI 7. The VEI 8 eruptions on this list predate our Holocene-focused database entirely — they occurred millions to tens of thousands of years ago — but they're well-documented through ignimbrite deposits, caldera dimensions, and tephra stratigraphy in the geological literature.
| # | Volcano | VEI | Volume | Date |
|---|
| 1 | La Garita Caldera (Fish Canyon Tuff)(Colorado, USA) | 8 | ~5,000 km³ | 28 million years ago |
| 2 | Toba(Sumatra, Indonesia) | 8 | ~2,800 km³ | 74,000 years ago |
| 3 | Huckleberry Ridge (Yellowstone)(Wyoming, USA) | 8 | ~2,450 km³ | 2.1 million years ago |
| 4 | Oruanui (Taupo)(New Zealand) | 8 | ~1,170 km³ | 25,700 years ago |
| 5 | Lava Creek (Yellowstone)(Wyoming, USA) | 8 | ~1,000 km³ | 640,000 years ago |
| 6 | Campanian Ignimbrite (Campi Flegrei)(Italy) | 7 | ~300 km³ | 39,000 years ago |
| 7 | Kurile Lake (Kamchatka)(Russia) | 7 | ~170 km³ | 6440 BC |
| 8 | Mount Mazama (Crater Lake)(Oregon, USA) | 7 | ~50 km³ magma | 5680 BC |
| 9 | Kikai(Japan) | 7 | ~170 km³ | 4350 BC |
| 10 | Santorini (Minoan Eruption)(Greece) | 7 | ~60 km³ | ~1610 BC |
| 11 | Samalas (Rinjani)(Lombok, Indonesia) | 7 | ~40 km³ magma | 1257 |
| 12 | Tambora(Indonesia) | 7 | ~150 km³ | 1815 |
| 13 | Krakatau(Indonesia) | 6 | ~25 km³ | 1883 |
| 14 | Novarupta(Alaska, USA) | 6 | ~15 km³ | 1912 |
| 15 | Pinatubo(Philippines) | 6 | ~10 km³ | 1991 |
The 15 Largest Eruptions — In Detail
For each eruption, I've included the volume ejected, VEI rating, and the Mount St. Helens multiplier — because “5,000 km³” doesn't mean much until you compare it to an eruption most people can picture. Every fact below is sourced from the Smithsonian GVP, USGS, or peer-reviewed geological research.
1La Garita Caldera (Fish Canyon Tuff) — Colorado, USA
VEI: 8Volume: ~5,000 km³Date: 28 million years agovs. St. Helens: 5,000x
The single largest eruption known to science. The Fish Canyon Tuff eruption created the La Garita Caldera in what’s now the San Juan Mountains of Colorado — a depression roughly 75 by 35 kilometers. The eruption ejected approximately 5,000 km³ of pyroclastic material, blanketing much of central North America in ash. To put that in perspective: that’s 4,800 times the volume of Mount St. Helens’ 1980 eruption. The ignimbrite deposits are so extensive that geologists mapped them across six US states before tracing them back to a single source caldera in the 1970s.
2Toba — Sumatra, Indonesia
VEI: 8Volume: ~2,800 km³Date: 74,000 years agovs. St. Helens: 2,800x
The largest eruption in the last 2 million years. Toba’s catastrophic VEI 8 event created Lake Toba — the world’s largest volcanic lake at 100 by 30 kilometers. Ash deposits reached 15 cm thick across the entire Indian subcontinent, and volcanic glass has been found in Greenland ice cores. For decades, the “Toba catastrophe theory” suggested this eruption nearly wiped out humanity, reducing our population to perhaps 10,000 individuals. But 2026 research from Curtis Marean’s team at Arizona State has largely debunked this: archaeological sites in Africa show continuous human occupation through the eruption. Humans didn’t nearly go extinct — they adapted.
3Huckleberry Ridge (Yellowstone) — Wyoming, USA
VEI: 8Volume: ~2,450 km³Date: 2.1 million years agovs. St. Helens: 2,450x
The first and largest of Yellowstone’s three caldera-forming super-eruptions. The Huckleberry Ridge Tuff covered much of the western United States in ash and created a caldera roughly 100 km long. This eruption marks the earliest known activity of the Yellowstone hotspot in its current position — though the hotspot itself has been active for at least 16 million years, leaving a trail of older calderas across southern Idaho as the North American Plate drifted southwest over it.
4Oruanui (Taupo) — New Zealand
VEI: 8Volume: ~1,170 km³Date: 25,700 years agovs. St. Helens: 1,170x
The most recent confirmed VEI 8 eruption on Earth, and the world’s largest known phreatomagmatic eruption — meaning groundwater played a major role in the explosive dynamics. The Oruanui event ejected over 1,170 km³ of material and devastated most of New Zealand’s North Island. The caldera it created now holds Lake Taupo. What makes Taupo especially noteworthy is that it didn’t stop there: its 232 CE eruption, while much smaller, produced pyroclastic flows traveling at 250–300 km/h across 20,000 km² — one of the most violent Holocene eruptions.
5Lava Creek (Yellowstone) — Wyoming, USA
VEI: 8Volume: ~1,000 km³Date: 640,000 years agovs. St. Helens: 1,000x
The eruption that created the Yellowstone Caldera as we know it today — the 72 by 55 kilometer depression that underlies Yellowstone National Park. The Lava Creek Tuff covers vast areas of the western US, and ash from this eruption has been identified as far east as the Gulf of Mexico. This was Yellowstone’s third and most recent caldera-forming eruption. Beneath the current caldera lies a magma reservoir containing roughly 46,000 km³ of partially molten rock — though only an estimated 5–15% is actually liquid.
6Campanian Ignimbrite (Campi Flegrei) — Italy
VEI: 7Volume: ~300 km³Date: 39,000 years agovs. St. Helens: 300x
The largest eruption in European history, and one that may have helped seal the fate of the Neanderthals. The Campanian Ignimbrite eruption deposited ash across the entire eastern Mediterranean, with layers found in Russia, North Africa, and the Black Sea floor. A 2010 study in Current Anthropology argued the eruption’s volcanic winter — combined with the broader climate cooling of Heinrich Event 4 — pushed already-declining Neanderthal populations past the point of recovery. The caldera it created is now Campi Flegrei, where 1.5 million people live today.
7Kurile Lake (Kamchatka) — Russia
VEI: 7Volume: ~170 km³Date: 6440 BCvs. St. Helens: 170x
One of Earth’s largest Holocene eruptions and among the least well-known on this list — largely because Kamchatka is one of the most remote volcanic regions on the planet. The eruption created Kurile Lake caldera in southern Kamchatka, depositing ignimbrite sheets across hundreds of square kilometers. In our database, this is one of only a handful of VEI 7 events in the Holocene. Kamchatka’s volcanic arc contains over 160 volcanoes, 29 of them active, making it one of the most volcanically dense regions on Earth.
8Mount Mazama (Crater Lake) — Oregon, USA
VEI: 7Volume: ~50 km³ magmaDate: 5680 BCvs. St. Helens: 50x
The eruption that created one of America’s most iconic landscapes: Crater Lake. Mount Mazama, once a ~3,700-meter stratovolcano, collapsed into its emptied magma chamber after ejecting roughly 50 km³ of magma (about 150 km³ as tephra). The resulting caldera filled with rainwater and snowmelt over centuries to create the deepest lake in the United States at 594 meters. Klamath tribal oral histories describe the eruption as a battle between the spirits of the sky and the underworld — one of the oldest geological oral traditions on record.
9Kikai — Japan
VEI: 7Volume: ~170 km³Date: 4350 BCvs. St. Helens: 170x
The largest Holocene eruption in Japan, and one with dire consequences for early Japanese civilization. The Kikai caldera eruption sent pyroclastic flows across the sea surface for over 100 km, devastating southern Kyushu and effectively wiping out the Jōmon culture in the region. Archaeological evidence shows a gap of centuries before the area was resettled. In March 2026, researchers from Kobe University confirmed that Kikai’s submarine caldera is actively recharging with new magma — a finding that has intensified monitoring efforts across Japan’s submarine volcanic arc.
10Santorini (Minoan Eruption) — Greece
VEI: 7Volume: ~60 km³Date: ~1610 BCvs. St. Helens: 60x
The eruption that destroyed the Minoan civilization on Crete and may have inspired the legend of Atlantis. The Minoan eruption of Thera (modern Santorini) generated tsunamis up to 35 meters high that struck Crete’s northern coast, where the Minoan palace of Knossos stood. Ash deposits have been found across the eastern Mediterranean, and the eruption likely caused short-term climate cooling visible in tree-ring records from Ireland to California. The caldera it created — now partially filled by the Aegean Sea — is one of the most photographed geological features in the world.
11Samalas (Rinjani) — Lombok, Indonesia
VEI: 7Volume: ~40 km³ magmaDate: 1257vs. St. Helens: 40x
The eruption that nobody knew about until 2013. For decades, ice core records showed a massive sulfur spike in 1258/1259 — the largest stratospheric sulfur injection of the Common Era — but nobody could identify the source. French volcanologist Franck Lavigne finally traced it to Mount Samalas, the predecessor of Rinjani’s caldera on Lombok. The eruption released an estimated 158 teragrams of SO₂ into the stratosphere, triggering global cooling that contributed to the Great Famine of 1258 in England and crop failures across Europe. Medieval chronicles describe foggy skies and failed harvests — but never named the cause.
12Tambora — Indonesia
VEI: 7Volume: ~150 km³Date: 1815vs. St. Helens: 150x
The most powerful eruption in recorded human history. Tambora’s April 1815 event ejected 150 km³ of material, lowered the mountain from 4,300m to 2,850m, and killed roughly 12,000 people directly through pyroclastic flows and ashfall. But the real catastrophe came after: so much sulfur dioxide entered the stratosphere that global temperatures dropped 0.4–0.7°C, producing the infamous “Year Without a Summer” in 1816. Crop failures across the Northern Hemisphere killed an estimated 80,000 through famine and disease. It caused the last great subsistence crisis in the Western world.
13Krakatau — Indonesia
VEI: 6Volume: ~25 km³Date: 1883vs. St. Helens: 25x
The loudest sound in recorded history. Krakatau’s August 27, 1883 eruption was heard 4,800 km away on Rodrigues Island near Mauritius — the equivalent of hearing a sound from New York in Dublin. The explosion generated a pressure wave that circled the globe 3.5 times, recorded on barographs worldwide. When two-thirds of the island collapsed into the emptied magma chamber, it triggered tsunamis up to 41 meters high that killed 36,000 people along the coasts of Java and Sumatra. The eruption also produced vivid red sunsets worldwide for months, which some art historians believe influenced Edvard Munch’s The Scream.
14Novarupta — Alaska, USA
VEI: 6Volume: ~15 km³Date: 1912vs. St. Helens: 15x
The largest eruption of the 20th century — and it happened where almost nobody was watching. Novarupta’s June 1912 eruption on the Alaska Peninsula ejected 15 km³ of magma in 60 hours, creating the Valley of Ten Thousand Smokes: a 40 km² plain of ash flow deposits up to 210 meters deep. Ash fell on Kodiak Island, 160 km away, for three days straight. Darkness was total. Remarkably, no one died — the area was virtually uninhabited. For decades, nearby Mount Katmai got the blame, but geological detective work in the 1950s proved that the actual vent was Novarupta, 10 km to the west.
15Pinatubo — Philippines
VEI: 6Volume: ~10 km³Date: 1991vs. St. Helens: 10x
The eruption that proved modern volcanology can save lives. When Pinatubo showed signs of unrest in April 1991, USGS and PHIVOLCS scientists correctly predicted a major eruption within weeks. Over 75,000 people were evacuated — including 15,000 US military personnel from Clark Air Base. The June 15 climactic eruption injected 17 megatons of SO₂ into the stratosphere, lowering global temperatures by 0.5°C for two years. Despite the eruption’s power, only 847 people died — mostly from roof collapses under rain-soaked ash during Typhoon Yunya, which struck simultaneously. Without the evacuation, the death toll would have been in the tens of thousands.
VEI Comparison — Using Mount St. Helens as a Baseline
Numbers like “2,800 km³” are hard to conceptualize. So here's a simpler way to think about these eruptions: Mount St. Helens' 1980 eruption ejected roughly 1 km³ of material. It killed 57 people, flattened 600 km² of forest, and sent ash across 11 US states. That's your baseline — 1x. Now multiply.
| Eruption | VEI | Volume | vs. St. Helens |
|---|
| Mount St. Helens (1980) | 5 | ~1 km³ | 1x (baseline) |
| Pinatubo (1991) | 6 | ~10 km³ | 10x |
| Krakatau (1883) | 6 | ~25 km³ | 25x |
| Tambora (1815) | 7 | ~150 km³ | 150x |
| Lava Creek / Yellowstone (640 ka) | 8 | ~1,000 km³ | 1,000x |
| Oruanui / Taupo (25.7 ka) | 8 | ~1,170 km³ | 1,170x |
| Huckleberry Ridge / Yellowstone (2.1 Ma) | 8 | ~2,450 km³ | 2,450x |
| Toba (74 ka) | 8 | ~2,800 km³ | 2,800x |
| Fish Canyon Tuff (28 Ma) | 8 | ~5,000 km³ | 5,000x |
That table should unsettle you a little. Pinatubo lowered global temperatures by 0.5°C and it was only 10x St. Helens. Tambora at 150x caused the worst famine of the 19th century. And the Fish Canyon Tuff? 5,000x. The scale of geological violence Earth is capable of is genuinely difficult to internalize.
Could a VEI 8 Eruption Happen Again?
Yes. The question isn't whether, it's when — and “when” almost certainly means not in our lifetimes. Here's where things actually stand at the four most-discussed candidates:
Three caldera-forming eruptions: 2.1 million, 1.3 million, and 640,000 years ago. The intervals are 800,000 and 660,000 years. That's not a regular cycle, and Yellowstone is not“overdue” despite what clickbait headlines claim. The current magma chamber is only 5–15% molten — far below the ~50% threshold most volcanologists believe is necessary for a caldera-forming eruption. The Yellowstone Volcano Observatory monitors it 24/7, and if that melt fraction started climbing, we'd see decades of escalating seismic unrest first. The annual probability of a VEI 8 Yellowstone eruption is approximately 1 in 730,000.
This is the one that genuinely concerns volcanologists. Campi Flegrei is a supervolcano caldera — the source of the Campanian Ignimbrite 39,000 years ago — and it sits under the western suburbs of Naples, with 1.5 million people in the danger zone. The caldera has been in a state of unrest since the 1950s, with accelerating ground uplift (bradyseism) and increasing seismic swarms. March 2026 research from INGV projects a potential critical transition between 2030 and 2034. That doesn't mean a super-eruption is imminent — a smaller eruption or continued unrest without eruption are both more likely — but Campi Flegrei demands serious attention.
Kikai produced the largest Holocene eruption in Japan (VEI 7, ~170 km³, 4350 BC) and devastated the Jōmon culture across southern Kyushu. In March 2026, Kobe University researchers confirmed that Kikai's submarine caldera is actively recharging with new magma. The dome growing inside the caldera contains a lava volume of roughly 32 km³. While a repeat of the 4350 BC eruption isn't expected soon, the confirmation of active magma supply means Kikai can't be written off as extinct.
Toba (Sumatra)
The source of the largest eruption in 2 million years still has a magma body beneath it — roughly 320 km² in area according to seismic tomography studies. The island of Samosir within Lake Toba has been slowly rising, indicating ongoing magmatic pressure. But 74,000 years is a very short interval by supervolcano standards, and most volcanologists consider another VEI 8 from Toba extremely unlikely for tens of thousands of years at minimum.
The Bottom Line
A VEI 8 eruption has roughly a 1 in 730,000 chance of occurring in any given year — a probability calculated by the Geological Society of London based on the frequency of past super-eruptions. We're far more likely to see a VEI 6 or VEI 7 event in our lifetimes. The last VEI 7 was Tambora in 1815. The last VEI 6 was Pinatubo in 1991. Statistically, another VEI 6 or 7 within the next century is a near-certainty. A VEI 8? Almost certainly not — but the supervolcanoes that could produce one are still very much alive.
What Makes an Eruption Massive?
Not all volcanoes are capable of producing the eruptions on this list. Three factors determine whether an eruption can reach VEI 7 or 8:
Magma volume and silica content.Super-eruptions require enormous magma chambers — typically hundreds to thousands of cubic kilometers of silica-rich (rhyolitic or dacitic) magma. High silica means high viscosity, which traps dissolved volcanic gases. When that pressure finally overcomes the confining rock, the eruption is explosive rather than effusive. This is why you'll never see a shield volcano like Kīlauea on this list — its low-silica basaltic magma flows instead of exploding.
Tectonic setting.Most of the eruptions on this list occurred at subduction zones or above mantle hotspots — settings that generate the silica-rich magmas needed for explosive eruptions. The Ring of Fire accounts for 75% of Earth's active volcanoes and the vast majority of VEI 5+ eruptions. Yellowstone and La Garita sit over continental hotspots, where plume-derived heat melts thick continental crust into enormous rhyolitic reservoirs.
Time.Super-eruptions require centuries to millennia of magma accumulation. The magma chamber beneath Yellowstone has been building for 640,000 years since the last caldera-forming event. These systems are patient. The eruptions themselves last hours to days, but the buildup takes geological time. That's actually good news: if a supervolcano begins ramping toward eruption, the precursory signals — ground uplift, increasing seismicity, changes in gas emissions — would likely be visible for decades.
Recorded History vs. Deep Time
There's a striking divide on this list. The top five eruptions all occurred tens of thousands to millions of years ago — we know them only from their geological deposits. The bottom five all happened within the last 800 years and were witnessed by humans. In between sits a gap of millennia where we rely on radiocarbon dating, ice core chemistry, and tree-ring anomalies to reconstruct what happened.
This matters because it means our understanding of truly large eruptions is fundamentally limited. We've never observed a VEI 8 eruption. We don't know exactly how one starts, how long it lasts, or what the precursory signals look like. Our best understanding comes from the ash deposits and pyroclastic flow remnants they left behind — frozen snapshots of events that reshaped continents.
The eruption of Vesuvius in 79 AD, often called the most famous eruption in history, didn't even make this list. At VEI 5, it ejected about 3.3 km³ — impressive, certainly deadly, but 1,500 times smaller than the Fish Canyon Tuff. That's the humbling reality of volcanic scale: the eruptions we remember are a rounding error compared to what Earth's geology has actually produced.
Explore Eruption Data for All 1,491 Volcanoes
Every volcano in our database with full eruption history, VEI data, and current alert status
Frequently Asked Questions
What was the largest volcanic eruption ever?
The largest volcanic eruption in Earth’s history was the Fish Canyon Tuff eruption at La Garita Caldera in present-day Colorado, approximately 28 million years ago. It ejected roughly 5,000 km³ of pyroclastic material — about 5,000 times the volume of Mount St. Helens’ 1980 eruption. It ranks as a VEI 8 event and created a caldera 75 by 35 km across.
What is the largest volcanic eruption in recorded human history?
The 1815 eruption of Mount Tambora in Indonesia is the largest eruption in recorded history, rated VEI 7 with approximately 150 km³ of material ejected. It killed 92,000 people (12,000 directly, 80,000 from famine) and caused the “Year Without a Summer” in 1816 by injecting massive quantities of sulfur dioxide into the stratosphere.
When was the last VEI 8 eruption?
The most recent VEI 8 (super-eruption) was the Oruanui eruption at Taupo, New Zealand, approximately 25,700 years ago. It ejected about 1,170 km³ of material. No VEI 8 eruption has occurred during recorded human history — all known super-eruptions predate written records by thousands to millions of years.
Could Yellowstone erupt again?
Yellowstone could theoretically produce another super-eruption, but it’s not “overdue” despite what clickbait headlines claim. The three caldera-forming eruptions occurred 2.1 million, 1.3 million, and 640,000 years ago — irregular intervals that don’t establish a predictable cycle. Current monitoring shows the magma chamber is only 5–15% molten, far below the threshold needed for a caldera-forming eruption. The USGS estimates the annual probability of a VEI 8 Yellowstone eruption at roughly 1 in 730,000.
What would happen if a VEI 8 eruption occurred today?
A VEI 8 eruption today would be a global catastrophe. Within days, pyroclastic flows would devastate everything within ~100 km. Ash would blanket thousands of square kilometers, collapsing buildings and making the region uninhabitable. Stratospheric aerosols would lower global temperatures by 5–10°C for years, causing widespread crop failures, famine, and economic collapse. Air travel worldwide would be disrupted for months. However, the probability of any VEI 8 eruption in a given year is approximately 1 in 730,000.
How many VEI 7+ eruptions are in the VolcanoDB database?
Our Smithsonian-sourced database contains 11,079 eruptions, of which 240 are rated VEI 5 or higher and 7 are confirmed VEI 7. VEI 8 eruptions occurred millions to tens of thousands of years ago and predate our Holocene-focused eruption records, but they are well-documented in the geological literature through ignimbrite deposits, caldera measurements, and tephra stratigraphy.