Tidal notches are a generally excepted sea-level marker. Particularly in the Mediterranean, those shoreline indicators are oftentimes used to infer coastal coseismic activity when they occur displaced from present day sea-level. Now, paleoseismologists should be able to visualize coastal evolution in order to better understand coseismic history. more
Posts in the category » « ( 286 Posts )
-
Use late-Holocene tidal notches as earthquake geological effects?
2017-05-30 | in Paper