Great Hanshin earthquake of northeastern Japan. The Great Hanshin earthquake belonged to a third type, called an "inland shallow earthquake". Earthquakes of this type occur along active faults. Even at lower magnitudes, they can be very destructive because they often occur near populated areas and because their hypocenters are located less than 20 km below the surface. The Great Hanshin earthquake began north of the island of Awaji, which lies just south of Kobe. It spread toward the southwest along the Nojima Fault on Awaji and toward the northeast along the Suma and Suwayama faults, which run through the center of Kobe. Observations
2011 Tōhoku earthquake and tsunami it is also assessed that a tsunami-earthquake with a tsunami magnitude scales (Mt) between 8.6 and 9.0 (Similar to 1896 Sanriku earthquake, the Mt for the 2011 Tōhoku earthquake is 9.1–9.4) will have a 30% chance to occur within 30 years. The quake gave scientists the opportunity to collect a large amount of data so as to model in great detail the seismic events that took place. This data is expected to be used in a variety of ways, providing as it does unprecedented information about how buildings respond to shaking, and other effects. Gravimetric data from the quake has