The high market-implied probability against a VEI 6 or greater eruption in 2026 reflects the low historical frequency of these events—roughly one every 50–100 years on average—and the current lack of detectable precursory signals from global monitoring networks. The most recent VEI 6 occurred in 1991 at Mount Pinatubo, and ongoing USGS and Smithsonian Institution data show no large-scale magmatic intrusions, significant caldera inflation, or seismic swarms at high-risk silicic systems that would indicate imminent escalation to that intensity. While an unexpected rapid buildup of pressure at a restless volcano could still occur, present observations place such an outcome well outside typical annual rates for the remainder of the year.
Résumé expérimental généré par IA à partir des données Polymarket. Ceci n'est pas un conseil de trading et ne joue aucun rôle dans la résolution de ce marché. · Mis à jourÉruption volcanique majeure (VEI ≥6) en 2026 ?
Éruption volcanique majeure (VEI ≥6) en 2026 ?
Oui
$80,401 Vol.
$80,401 Vol.
31 mars 2027
Oui
$80,401 Vol.
$80,401 Vol.
31 mars 2027
This market will resolve to "Yes" if a natural volcanic eruption with a Volcanic Explosivity Index (VEI) of 6 or higher occurs between the market's creation and December 31, 2026, 11:59 PM ET. Otherwise, this market will resolve to “No”.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.The high market-implied probability against a VEI 6 or greater eruption in 2026 reflects the low historical frequency of these events—roughly one every 50–100 years on average—and the current lack of detectable precursory signals from global monitoring networks. The most recent VEI 6 occurred in 1991 at Mount Pinatubo, and ongoing USGS and Smithsonian Institution data show no large-scale magmatic intrusions, significant caldera inflation, or seismic swarms at high-risk silicic systems that would indicate imminent escalation to that intensity. While an unexpected rapid buildup of pressure at a restless volcano could still occur, present observations place such an outcome well outside typical annual rates for the remainder of the year.
This market will resolve to "Yes" if a natural volcanic eruption with a Volcanic Explosivity Index (VEI) of 6 or higher occurs between the market's creation and December 31, 2026, 11:59 PM ET. Otherwise, this market will resolve to “No”.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.
Marché ouvert : Dec 29, 2025, 6:24 PM ET
Volume
$80,401Date de fin
31 mars 2027Marché ouvert
Dec 29, 2025, 6:24 PM ETResolver
0x65070BE91...This market will resolve to "Yes" if a natural volcanic eruption with a Volcanic Explosivity Index (VEI) of 6 or higher occurs between the market's creation and December 31, 2026, 11:59 PM ET. Otherwise, this market will resolve to “No”.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.The high market-implied probability against a VEI 6 or greater eruption in 2026 reflects the low historical frequency of these events—roughly one every 50–100 years on average—and the current lack of detectable precursory signals from global monitoring networks. The most recent VEI 6 occurred in 1991 at Mount Pinatubo, and ongoing USGS and Smithsonian Institution data show no large-scale magmatic intrusions, significant caldera inflation, or seismic swarms at high-risk silicic systems that would indicate imminent escalation to that intensity. While an unexpected rapid buildup of pressure at a restless volcano could still occur, present observations place such an outcome well outside typical annual rates for the remainder of the year.
This market will resolve to "Yes" if a natural volcanic eruption with a Volcanic Explosivity Index (VEI) of 6 or higher occurs between the market's creation and December 31, 2026, 11:59 PM ET. Otherwise, this market will resolve to “No”.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.
The primary resolution source will be the Smithsonian Institution Global Volcanism Program (GVP: https://volcano.si.edu/), specifically the ‘VEI 6’ figure for 2026 released on the page currently titled "Eruptions Avg 2000-2024 (N/T)" (https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear) as of March 31, 2027, 12 PM ET. Any prior updates will not be considered finalized.
If this dataset has not been updated to include all relevant events by March 31, 2027, or if the Smithsonian GVP becomes permanently unavailable, this market may resolve based on a consensus of credible scientific sources, including the U.S. Geological Survey (USGS), national or regional volcanic observatories, or credible reporting of a scientific consensus.
Note: Smithsonian Institution Global Volcanism Program databases, which include eruptions that reached the relevant threshold prior to this market’s timeframe (e.g., https://volcano.si.edu/faq/index.cfm?question=eruptionsbyyear&checkyear=2025), will not be considered.
Volume
$80,401Date de fin
31 mars 2027Marché ouvert
Dec 29, 2025, 6:24 PM ETResolver
0x65070BE91...The high market-implied probability against a VEI 6 or greater eruption in 2026 reflects the low historical frequency of these events—roughly one every 50–100 years on average—and the current lack of detectable precursory signals from global monitoring networks. The most recent VEI 6 occurred in 1991 at Mount Pinatubo, and ongoing USGS and Smithsonian Institution data show no large-scale magmatic intrusions, significant caldera inflation, or seismic swarms at high-risk silicic systems that would indicate imminent escalation to that intensity. While an unexpected rapid buildup of pressure at a restless volcano could still occur, present observations place such an outcome well outside typical annual rates for the remainder of the year.
Résumé expérimental généré par IA à partir des données Polymarket. Ceci n'est pas un conseil de trading et ne joue aucun rôle dans la résolution de ce marché. · Mis à jour
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