How good are our current seafloor maps?
- Associate Professor in Global Seismology, University of Bristol
El interior de nuestro planeta es un rompecabezas que no resulta fácil resolver. Un nuevo estudio aporta luz sobre la edad del núcleo y la historia alrededor del campo magnético de la Tierra.
8,000 tonnes of molten iron solidifies in Earth’s inner core every second – but it’s not distributed equally.
Mars’ core is larger and less dense than we thought.
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