📰
Sourced From
Phys.org
Read Full Article →

Since scientists can't drill 2,900 km (1,800 miles) to the boundary between Earth's core and deep mantle, they must use information relayed by seismic waves recorded during earthquakes to study this region. In a new study published in the journal JGR…

Source: Phys.orgRead full article →


Content sourced from third parties. Copyright belongs to original publishers.


Leave a Reply

Your email address will not be published. Required fields are marked *