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The Bismarck volcanic arc, New Britain, and the Taupō Volcanic Zone, New Zealand, appear often too. In addition to the events listed below, there are many examples of eruptions in the Holocene on the Kamchatka Peninsula, [3] which are described in a supplemental table by Peter Ward. [4]
The volcanic ash fall pelted the capital and La Aurora International Airport. The National Coordinator for Disaster Reduction (CONRED) declared a red alert for the communities near the volcano and recommended the evacuation of some of them. Noti7 reporter Anibal Archila, one of the first to cover the event, was reportedly killed by volcanic debris.
Dieng Volcanic Complex: 2 Indonesia: 1928 [30] 39 Taal: 4 Philippines: 2020 2020–2022 Taal Volcano eruptions: 38 Dieng Volcanic Complex: 2 Indonesia: 1786 [30] 32 Mount Nyiragongo: 1 Democratic Republic of the Congo: 2021 2021 Mount Nyiragongo eruption: 32 Kelud: 4 Indonesia: 1990 [40] 31 Bayonnaise Rocks: 2 Japan: 1952 [41] 31 Nabro Volcano ...
Volcano/complex Volcanic arc/belt, subregion, or hotspot Material volume (km 3) Age in Ka [1] Tephra or eruption name 6 Lolobau Island: Bismarck Volcanic Arc 50 12 caldera formation 6 Menengai: Great Rift Valley, Kenya < 25 12.3 Ruplax Tuff 6 Nevado de Toluca: Trans-Mexican Volcanic Belt: 20 12.5 Upper Toluca Pumice 6 Sakurajima: Kyūshū: 11 12.8
Satellite images of the 15 January 2022 eruption of Hunga Tonga-Hunga Haʻapai. This is a list of volcanoes that have had large explosive eruptions during the Holocene (since about 11,650 years Before Present), with a volcanic explosivity index (VEI) of 5 or higher, or a plume height of at least 30 km.
In a volcanic eruption, lava, volcanic bombs, ash, and various gases are expelled from a volcanic vent and fissure. While many eruptions only pose dangers to the immediately surrounding area, Earth's largest eruptions can have a major regional or even global impact, with some affecting the climate and contributing to mass extinctions.
This is a list of notable volcanic eruptions in the 16th to 20th centuries with a Volcanic explosivity index (VEI) of 4 or higher, and smaller eruptions that resulted in significant damage or fatalities. Note that there may be uncertainties to dates with historical eruptions, and there are likely to be many large eruptions that have not been ...
Unknown; may include climate changes, massive volcanic eruptions and Humans (largely by human overhunting) [4] [5] [6] Neogene: Pliocene–Pleistocene boundary extinction: 2 Ma: Possible causes include a supernova [7] [8] or the Eltanin impact [9] [10] Middle Miocene disruption: 14.5 Ma Climate change due to change of ocean circulation patterns.