Tsunamis

Following certain earthquakes, very long-wavelength water waves in oceans or seas sweep inshore. More properly called seismic sea waves or tsunamis (tsunami is a Japanese word for “harbour wave”), they are commonly referred to as tidal waves, although the attractions of the Moon and Sun play no role in their formation. They sometimes come ashore to great heights—tens of metres above mean tide level—and may be extremely destructive.

For more: http://sciaeon.org/geology-and-geoscience/home

For Manuscript submission: http://www.sciaeon.org/submit-paper

For contact: radiology@sciaeonopenaccess.com

Leave a Reply

Create your own website, free on WordPress.com.Create your own website.
Start free