List of Quaternary volcanic eruptions
This article is a list of historical volcanic eruptions of approximately magnitude 6 or more on the Volcanic Explosivity Index or equivalent sulfur dioxide emission during the Holocene, and Pleistocene eruptions of the Decade Volcanoes ; Campania, Italy; South Aegean Volcanic Arc; Laguna de Bay, Luzon Volcanic Arc; Mount Pinatubo, Luzon Volcanic Arc; Toba, Sunda Arc; Mount Meager massif, Garibaldi Volcanic Belt; Yellowstone hotspot, Wyoming; and Taupō Volcanic Zone, greater than VEI 4.
The eruptions in the Holocene on the link: were not added yet, but they are listed on the Peter L. Ward's supplemental table. Some of the eruptions are not listed on the Global Volcanism Program timetable as well, at least not as VEI 6. The timetables of Global Volcanism Program; Bristlecone pine tree-rings ; the 4 ka Yamal Peninsula Siberian larch chronology; the 7 ka Scots pine chronology from Finnish Lapland; GISP2 ice core; GRIP ice core; Dye 3 ice core; Bipolar comparison; Antarctic ice core ; Antarctic ice core ; Crête ice core, in central Greenland, benthic foraminifera in deep sea sediment cores, do not agree with each other sometimes. The 536–547 AD dust-veil event might be an impact event.
Holocene eruptions
The Holocene epoch begins 11,700 years BP,1 to 1000 AD
| Tianchi eruption, Paektu Mountain, border of North Korea and China | 946 AD | 6 | of tephra | Also known as Millennium Eruption of Changbaishan |
| Eldgjá eruption, Laki system, Iceland | 934–940 AD | 6 | Estimated of lava | Estimated 219 million tons of sulfur dioxide were emitted |
| Ceboruco, Northwest of the Trans-Mexican Volcanic Belt | 930 AD ±200 | 6 | of tephra | |
| Dakataua, Northern tip of the Willaumez Peninsula, New Britain, Papua New Guinea | 800 AD ±50 | 6? | ? of tephra | |
| Pago, East of Kimbe, New Britain, Papua New Guinea: Witori Caldera | 710 AD ±75 | 6 | of tephra | |
| Mount Churchill, eastern Alaska | 700 AD ±200 | 6 | of tephra | |
| Rabaul, Rabaul Caldera, New Britain | 540 AD ±100 | 6 | of tephra | Volcanic winter of 536? |
| Ilopango, El Salvador | 431 AD ±2, or 539/540 AD | 7 | 106.5 km3 of tephra | |
| Ksudach, Kamchatka Peninsula, Russia | 240 AD ±100 | 6 | of tephra | |
| Taupō Volcanic Zone, Hatepe eruption of Taupō Volcano, New Zealand | 230 AD ±16 | 7 | of tephra | |
| Mount Vesuvius, Italy | 79 AD Oct 24 | 5? | of tephra | Pompeii eruption |
| Mount Churchill, eastern Alaska | 60 AD ±200 | 6 | of tephra | |
| Ambrym, Vanuatu | 50 AD ±100 | 6 | of tephra |
Pleistocene eruptions
2.588 ± 0.005 million years BP, the Quaternary period and Pleistocene epoch begin.| Name and area | Date | VEI | Products | Notes | - |
| GISP2 ice core event | 12.657 ka | - | |||
| Eifel hotspot, Laacher See, Vulkan Eifel, Germany | 12.900 ka | 6 | of tephra. | - | |
| Mount Vesuvius, Italy | 16 ka | 5 | Green Pumice | - | |
| Mount Vesuvius, Italy | 18.3 ka | 6 | Basal Pumice | - | |
| Santorini, Greece: Cape Riva Caldera | about 21 ka | - | |||
| Aira Caldera, south of the island of Kyūshū, Japan | about 22 ka | 7 | more than of tephra. | - | |
| Taupō Volcanic Zone, Oruanui eruption, Taupō Volcano, New Zealand | around 25.6 ka | 8 | Approximately of tephra | - | |
| Laguna Caldera, South-East of Manila, island of Luzon | 27–29 ka | - | |||
| Alban Hills, Rome, Italy | 36 ka | 4 | Peperino Ignimbrite of Albano Maar | Sedimentation and mobility of PDCs: a reappraisal of ignimbrites’ aspect ratio | |
| Campi Flegrei, Naples, Italy | 39.280 ka ± 0.11 | 200 cubic kilometres of lava | Campanian Tuff | - | |
| Galeras, Andes, Northern Volcanic Zone, Colombian department of Nariño | 40 ka | of tephra | - | ||
| Taupō Volcanic Zone, Rotoiti Ignimbrite, North Island, New Zealand | about 50 ka | 7 | about of tephra. | - | |
| Santorini, Greece: Skaros Caldera | about 70 ka | - | |||
| Lake Toba, Sumatra, Indonesia | 73.7 ka ± 0.3 | 8 | of tephra | estimated 150 to 1,000 million tons of sulfur dioxide were emitted. | - |
| Aso Caldera, Kumamoto Prefecture, Japan | 90 ka | 8 | of tephra | The largest known eruption in Japan | - |
| Yellowstone hotspot: Yellowstone Caldera | between 70 and 150 ka | intracaldera rhyolitic lava flows. | - | ||
| Galeras, Andes, Northern Volcanic Zone, Colombian department of Nariño | 150 ka | of tephra | - | ||
| Kos-Nisyros Caldera, Greece | 161 ka | Kos Plateau Tuff. | - | ||
| Taal Caldera, island of Luzon, Philippines | between 500 and 100 ka | 6 | ? | 6 Explosive Eruptions formed multiple overlapping calderas. | - |
| Santorini, Greece: Southern Caldera | about 180 ka | - | |||
| Taupō Volcanic Zone, Rotorua Caldera, New Zealand | 220 ka | more than of tephra. | - | ||
| Taupō Volcanic Zone, Maroa Caldera, New Zealand | 230 ka | of tephra. | - | ||
| Taupō Volcanic Zone, Reporoa Caldera, New Zealand | 230 ka | 7 | around of tephra | - | |
| Taupō Volcanic Zone, Whakamaru Caldera, North Island, New Zealand | around 254 ka | 8 | of tephra | Whakamaru Ignimbrite/Mount Curl Tephra | - |
| Taupō Volcanic Zone, Matahina Ignimbrite, Haroharo Caldera, North Island, New Zealand | 280 ka | 7 | about of tephra. | - | |
| Alban Hills, Rome, Italy | 365–351 ka | 6 | Villa Senni Ignimbrite >50km3 | Volcanoes of the World: Third Edition | |
| Sabatini volcanic complex, Sabatini, Italy | 374 ka | 7 | more than | Morphi tephra. | - |
| Roccamonfina Caldera, Roccamonfina, Italy | 385 ka | of tephra. | - | ||
| Alban Hills, Rome, Italy | 407–398 ka | 6 | Pozzolane Nere Ignimbrite | - | |
| Alban Hills, Rome, Italy | 456–439 ka | 7 | Pozzolane Rosse Tephritic Ignimbrite >50km3 | Sedimentation and mobility of PDCs: a reappraisal of ignimbrites’ aspect ratio | |
| Maipo (volcano), Andes, Southern Volcanic Zone, Chile | 450–500 ka | 7 | Diamante Caldera | - | |
| Galeras, Andes, Northern Volcanic Zone, Colombian department of Nariño | 560 ka | of tephra | - | ||
| Lake Toba, Sumatra, Indonesia | 501 ka ±5 | Middle Toba Tuff | - | ||
| Yellowstone hotspot: Yellowstone Caldera | 640 ka | 8 | more than of tephra | Lava Creek Tuff | - |
| Lake Toba, Sumatra, Indonesia | 840 ka ±30 | Oldest Toba Tuff | - | ||
| Taupō Volcanic Zone, Mangakino Caldera, North Island, New Zealand | 0.97 Ma | more than | Rocky Hill Ignimbrite | - | |
| Taupō Volcanic Zone, Mangakino Caldera, North Island, New Zealand | 1.01 Ma | more than | Unit E | - | |
| Lake Toba, Sumatra, Indonesia | 1.2 ±0.16 Ma | Haranggoal Dacite Tuff | - | ||
| Taupō Volcanic Zone, Mangakino Caldera, North Island, New Zealand | 1.23 Ma | more than | Ongatit Ignimbrite | - | |
| Yellowstone hotspot: Henry's Fork Caldera | 1.3 Ma | 7 | Mesa Falls Tuff. | - | |
| Yellowstone hotspot: Island Park Caldera | 2.1 Ma | 8 | Huckleberry Ridge Tuff. | - | |
| Cerro Galán Caldera, Argentina | 2.2 Ma | 8 | of dacitic magma. | - |
Nomenclature
Each state/ country seem to have a slightly different approach, but there is an order:- Craton, and then Province as sections or regions of a craton.
- First: volcanic arc, volcanic belt and volcanic zone.
- Second: volcanic area, caldera cluster and caldera complex.
- Third: volcanic field, volcanic system and volcanic center.
- * A volcanic field is a localized area of the Earth's crust that is prone to localized volcanic activity.
- * A volcanic group is a collection of related volcanoes or volcanic landforms.
- Neutral: volcanic cluster and volcanic locus.