News from the Geoblogosphere
New from Snet: Lithologs
, a new tool to create lithological/sedimentological logs online..
Monday, 27 April 2015
This zone is 200 km long. A true M8 would be 300 km long. The footwall is probably to the north, and all the populated areas are on the hanging wall, where all the aftershocks are. We are lucky the city wasn't in the true 'hammer zone' of the thrust fault. This happened with the Armenian earthquake, which was only an M7 but the city was on the zone.
Same with Kobe -- an M7 with
I have made the following decision on the future of my geophone network that I am currently running in Iceland. Next year (2016) I am going to do the following changes to it. Böðvarshólar geophone station is going … Continue reading