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This tectonic line consists of many active faults (e.g. Research Group for Active Faults 1991).
Northeastern Japan is one of the most tectonically active regions, having many active faults and volcanoes.
Geological formations there are intricately deformed and displaced by many active faults.
On the other hand, according to their maps, the positions of many active faults in the northern Sagami Trough are related to the positions of the knolls.
On the other hand, since the fracture is developed in the southwestern part of Ioto, where there are many active faults, phreatic eruption tends to occur.
Thus, lower shear strengths are maintained by materials with small grain sizes and strain localization should be a common feature for many active faults.
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As shown in Fig. 1, there are many Quaternary active faults in and around this zone.
In north-central Japan, the high strain rate zone includes many Quaternary active faults and volcanoes (Fig. 1).
This area was very tectonic-active with many folds and active faults trending NW SE (Figure 1).
Although reactors need to be near a large body of water for cooling purposes, there are many such locations without active faults.
Thus, many earthquakes have occurred along the active faults in this area (Sagiya 1999), including the AD 1930 North Izu earthquake (M 7.3; Tanna Fault) and the AD 1974 Off-Izu Peninsula earthquake (M 6.9; Irozaki Fault).
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