The inner core of our planet is between 1 and 1.3 billion years old, according to new research led by the University of Texas at Austin and Carnegie Institution for Science. Earth’s internal structure: dense solid metallic core, viscous metallic outer core, mantle and silicate based crust. Image credit: NASA. “People are really curious and excited about knowing about the origin of the geodynamo, the strength of the magnetic field, because they...
