Speaker: Mr Michael Anenburg (RSES)
Carbonatites are unusual igneous rocks that primarily contain carbonate minerals such as calcite or dolomite.
Speaker: Hrvoje Tkalčić (RSES)
More than 75 years ago, the Earth’s core was hypothesized to be solid in the centre as a result of a liquid–solid phase change in iron, which implies that shear waves in its sol
Speaker: Jess Amies (RSES)
The Mediterranean has great potential for reconstructing past climate due to high sedimentation rates and amplified climate signals.
Speaker: Alexander Piotrowski (University of Cambridge)
Ocean circulation plays a key role in the Earth’s climate system because surface ocean currents transport heat and deep ocean water masses can sequester carbon dioxide from the
Speaker: Zachary Sharp (University of New Mexico), The Mineralogical Society of America 2018 Distinguished Lecturer
Please note, this special school seminar is on a Wednesday.