Giant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.
Giant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.
Deep within Earth’s mantle lie two enormous, continent-sized structures known as LLVPs. Scientists once believed these ...
Scientists now know how to drill deep enough to tap into an energy supply that would power the world for more than 20 million ...
The Earth is made of different layers: the core, mantle and crust. Plate tectonic theory shows that the crust of the Earth is split into plates (pieces of the Earth’s crust). The movement of ...
The Earth's hidden ocean is 700 km beneath this continent. Scientists made a discovery that changes everything we thought we ...
A new study of decades worth of seismogram data shows that the surface of Earth’s iron and nickel core is more malleable than scientists thought.
A groundbreaking study reveals that the Moon has a solid inner core with a density comparable to iron, reshaping our ...