From San Francisco, at a meeting of the American Geophysical Union
New seismic observations are filling in scientists’ knowledge about the thickness of Earth’s crust, especially in the Southern Hemisphere.
Because vibrations traveling through any material are deflected by its irregularities, scientists can use seismic waves traveling through our planet to examine its structure.
Log in
Subscribers, enter your e-mail address for full access to the Science News archives and digital editions.