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Spying on open vent volcanoes from ground, air and space
13 June:7:45 pm - 9:30 pm
Talk by Dr. Emma Nicholson (Liu), University College London
Abstract:
“Open vent” volcanoes are persistently active and maintain an unbroken connection between shallow magma reservoirs and the atmosphere. These volcanoes are true natural laboratories, providing an unparalleled window into the subsurface physical and chemical processes that control volcanic activity. Open vent volcanoes sustain large volcanic gas emissions and are therefore the “chimney pipes” of our planet, responsible for shaping the Earth’s atmosphere over geological time and impacting regional air and water quality on human timescales. Lava lakes are rare end-members in the expressions of open vent volcanism and can remain stable for years to decades. Yet, recent events at Kilauea (Hawaii), Ambrym (Vanuatu) and Nyiragongo (DRC) have emphasized how rapidly these lakes can drain to feed voluminous flank eruptions, posing substantial environmental and societal hazards. I will review some of the recent advances and outstanding questions in our understanding of the mechanisms and impacts of open vent volcanic activity. In particular, I will focus on how remote sensing observations—from the ground, air and space—combined with studies of erupted volcanic rocks are providing new perspectives on the long-term eruptive behaviour of open vent volcanoes. This talk will draw on new insights from a National Geographic expedition to one of the most remote active volcanoes on Earth – Mt Michael, located in the South Sandwich Islands at the gateway to the Southern Ocean.
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