Calculated Coulomb stress change (along optimally-oriented strike slip faults at 10 km depth with friction of 0.4) is shown at left. Seismicity rate change after the M 7.1 quake is shown at right, in which warm colors indicate rate increases (aftershocks), and turquoise colors indicate rate decreases. Rate decreases are difficult to detect in the weeks after the mainshock.
ډیری عوامل افغاني ټولنې د زلزلې پر وړاندې زیانمنوي- August 11, 2022
- What’s happening this week in Humboldt County, California: The squeeze - February 6, 2019
- Finding of the unexpected tsunami due to the strike-slip fault at central Sulawesi, Indonesia on 28 September 2018, from the preliminary field survey at Palu - October 15, 2018