Unlike the classic Jules Verne science fiction novel Journey to the Center of the Earth or movie The Core, humans cannot venture into the Earth’s interior beyond a few kilometers of its surface. But thanks to latest advances in computer modelling, an international team of researchers led by the University of Bristol has shed new light on the properties and behavior of magma found several hundreds of kilometers deep within the Earth.
The study showed water-rich (hydrous) magmas (extremely hot liquid rocks) formed in the Earth’s mantle – the layer beneath its crust – are more buoyant and fluid than previously believed. This discovery allows us to predict how and where hydrous magmas move within Earth’s interior, which means the amount of water in these realms can be more reliably predicted, furthering understanding of the deep Earth water cycle.