Display listing of nearby significant earthquakes

There was a very strong earthquake and a moderate tsunami with source on the shelf of the Sea of Japan (several tens of kilometers to the north-northeast of Niigata) in the form of an ellipse measuring 90 x 35 km, extending along Honshu Island. The length of the zone of perceptibility was 1000 km.

The total losses from the earthquake and tsunami (separate figures for each phenomenon are not available) have been estimated at 80 million dollars; 26 people died and about 450 were injured; about 86,400 people suffered material losses.

The bulk of the damage occurred at Niigata. The seismic tremors themselves did slight damage to the city, except that a fire lasting two weeks broke out in the region of the oil tanks.

However, as the result of the seismic shocks there was an almost instantaneous compaction, with fractures, of the loose delta deposits of the Shinano and Agano Rivers, on which a large part of the city is located. An abrupt increase in the pressure of ground waters at a depth of about 1 m, caused the appearance of numerous mud volcanoes, which ejected a mixture of sand and water. This, together with other circumstances, led to the flooding of the soil. The upper loose layer liquesced. Multi-story buildings made of prestressed concrete and other tall structures with weak foundations inclined 5-15^o from the vertical, and some lay completely on the ground. Heavy buildings sank into the ground. The ends of long buildings shifted 1-2 m relative to each other.

The cause of the earthquake was the upward dislocation along tectonic fractures of a system of interlocked Neogene - Quaternary anticlinals, including the small rocky Ava Island, and the simultaneous settling of the narrow underwater depression, separating the above mentioned system from Honshu Island. Thus the dislocations in the earthquake corresponded to the general direction of the most recent tectonic movements in its focal zone. Quantitatively, these dislocations characterized by the following figures. Ava Island rose 1-1.5 m and tilted 1 deg to the northwest. The maximum elevation occurred on the floor of the sea 15 km south of Ava Island and was 5-6 m. The maximal local subsidence, near Honshu Island, was estimated at 3-4 m. In area, the zone of subsidences was approximately one tenth the area of elevations. These measurements of the floor tie in well with the results of the determination of the mechanism of the source of the earthquake on the basis of instrumental seismic data. The coast of Honshu Island adjoining the zone of subsidences subsided 10-20 cm. According to the tide gauge data, the slow tectonic movements in the focal zone in the four years before the earthquake were directed oppositely to the dislocations, but before and after this period, they had the same direction. On the basis of geomorphological observations, Japanese specialists surmise that about 800 years was required to prepare for the earthquake [this may be exaggerated]. The tsunami was maximal on the coast of Honshu Island closes to its source.

(above from Reference #414)

1,960 houses destroyed, 290 houses burned down. (reference #150)

June 16, 1964, 04:01:44.3 UTC, 38.3 N, 139.1 E, magnitude 7.25-7.5, depth about 57 km. 26 killed, 447 injured, and extensive property damage at Niigata. Tsunami observed along coastal areas. (reference #45)