Carbon-omics and global health
17 November 2023Cambridge Zero to host two research symposia to discuss critical climate change challenges
Cambridge Zero to host two research symposia to discuss critical climate change challenges
After centuries without volcanic activity, Iceland’s Reykjanes peninsula sprang to life in 2021 when lava erupted from the Fagradalsfjall volcano. New research involving the University of Cambridge helps us see what is going on deep beneath the volcano by reading the chemistry of lavas and volcanic gases almost as they were erupted.
Scientists from Cambridge University and NTU Singapore have found that slow-motion collisions of tectonic plates drag more carbon into Earth’s interior than previously thought.
Microscopic imperfections in rock crystals deep beneath Earth’s surface play a deciding factor in how the ground slowly moves and resets in the aftermath of major earthquakes, says new research involving the University of Cambridge.
A team of volcanologists who observed the colossal 2018 eruption of Kīlauea, Hawai’i, have tracked how potentially toxic metals carried in its gas plumes were transported away from the volcano to be deposited on the landscape.
New research led by the University of Cambridge has found rare evidence – preserved in the chemistry of ancient rocks from Greenland - which tells of a time when Earth was almost entirely molten.
Professor Marian Holness leads a research group in the Department of Earth Sciences, and studies the processes which occur during the melting and solidification of rocks. Here, she tells us how time spent in quiet activities like running, knitting and even breastfeeding have helped to trigger new insights in her research.
Dr Helen Williams is a Reader in Cambridge's Department of Earth Sciences and a Fellow of Jesus College. Here, she tells us about using rocks as pieces of forensic evidence, what it's like hundreds of kilometres below the Earth's surface, and why Cambridge brings out the best in her.
The molten rock that feeds volcanoes can be stored in the Earth’s crust for as long as a thousand years, a result which may help with volcanic hazard management and better forecasting of when eruptions might occur.
The chemical composition of gases emitted from volcanoes – which are used to monitor changes in volcanic activity – can change depending on the size of gas bubbles rising to the surface, and relate to the way in which they erupt. The results, published in the journal Nature Geoscience, could be used to improve the forecasting of threats posed by certain volcanoes.