The tsunami, which was generated by the earthquake, traveled across the Pacific Ocean and reached the Japanese island of Honshu, causing significant damage to coastal areas. The Japan Meteorological Agency (JMA) issued a tsunami warning for the entire country, urging people to evacuate to higher ground. The earthquake, which occurred at 8:17 AM JST, was felt across Japan, causing widespread panic and disruption. The tsunami, which was recorded at 10:00 AM JST, was the result of the earthquake’s energy being released into the ocean, causing a series of waves to form. The earthquake’s epicenter was located about 100 kilometers north of Torishima, a volcanic island in the Pacific Ocean. The tsunami’s height was measured at 50 centimeters, which is relatively low compared to the destructive power of tsunamis. However, it was still significant enough to cause damage to coastal areas.
The connection between the recent earthquake and the eruption of Smith Island remains unclear.
The agency’s assessment of the earthquake’s potential for causing a tsunami is based on the location of the epicenter, the depth of the earthquake, and the geological history of the region. These factors are used to determine the potential for a tsunami to occur. The agency’s assessment is based on a combination of scientific data and expert judgment. The agency’s experts have been monitoring the earthquake and its potential for causing a tsunami for several days. They have been analyzing data from seismic sensors, tide gauges, and other sources.