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As a rule, the cooling influence of an individual volcano will dominate for the period immediately after the eruption but the warming impact will last much longer.
LaMEVE can identify knowledge gaps and constrain return periods of explosive eruptions of different magnitudes on global, regional and local (individual volcano) scales.
At the individual volcano level, 41% of QEAR volcanoes only contribute one eruption (10% of all eruptions); the most eruptions contributed by a single volcano is 52 eruptions.
Power-law distributions represent self-similar properties in the eruption system and suggest there is no characteristic scale, even in an individual volcano.
Probability thresholds for a set consequence (e.g., life safety) could be pre-determined by end-users for each region or individual volcano, to assist with the determination of risk levels by scientists.
When an individual volcano is selected from the initial results page, a volcano summary, which includes a location map, is displayed at the top of the page (this is in addition to the full search results listed).
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Cinder cones also form at some vents on shield volcanoes, but these are not considered to be separate, individual volcanoes.
Volcanism as a syn-tectonic phenomenon may modify any landscape by fissure-erupted flood basalts capable of creating regional lava plateaus or by vent eruptions that yield individual volcanoes.
That allows geologists to supplement the necessarily patchy records they build up by studying individual volcanoes with an independent record of eruptions that have been large enough to change the climate.Our briefing, marking the 200th anniversary of Tambora the most powerful eruption in modern history assesses the risk of similar events happening again, at almost any time.
Calculated eruption rates vary greatly (101 10−4 km3 dense-rock equivalent/1000 years) between individual volcanoes.
However, individual volcanoes contribute anywhere from 1 to 52 eruptions (Fig. 1).
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