Tanna Fault

We recommend taking your children to visit.

Original Text

It is a fault park that occurred on November 26, 1930 due to the Kitaizu earthquake, which is directly below the magnitude 7.3. The shape of the stream in the park will be shifted on the way. It seems that this was a round garbage dump, but it shifted to the left and right due to the earthquake and became this shape. You can see the intensity of the earthquake well. There is a "fault underground observation room" in the corner of the park. We recommend taking your children to visit.

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Original Text

The Tana fault is a place where you can see the fault just by looking at it. It's free, but there's nothing more than checking the fault, and you can see it in 5 or 10 minutes.

The deviation of the fault is obvious at a glance! With your child.

Original Text

The Tana Fault in the idyllic Tana Basin. The deviation of the fault caused by the Kita Izu earthquake is preserved. Since there is a description of the fault, you can fully know about the Tana fault. I think that children in elementary school can observe it with interest, so it's a good idea to visit when you visit nearby Oracche.

The cause of the earthquake is preserved.

Original Text

You can see the Tana Fault, which caused the Kita Izu earthquake in 1930, and the deviation of the fault in Tana Fault Park. Since this fault is a lateral deviation fault, the place where the original 々 straight line is cut off sideways is preserved.

where the memory of the earthquake does not weather.

Original Text

It is about 20 minutes by car from JR Kannan Station. The deviation of the fault caused by the Kita Izu earthquake that occurred in 1945 is preserved and can be observed.