1923 Great Kantō earthquake and Great Hanshin earthquake

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between 1923 Great Kantō earthquake and Great Hanshin earthquake

1923 Great Kantō earthquake vs. Great Hanshin earthquake

The struck the Kantō Plain on the Japanese main island of Honshū at 11:58:44 JST (02:58:44 UTC) on Saturday, September 1, 1923. The, or Kobe earthquake, occurred on January 17, 1995 at 05:46:53 JST (January 16 at 20:46:53 UTC) in the southern part of Hyōgo Prefecture, Japan, known as Hanshin.

Similarities between 1923 Great Kantō earthquake and Great Hanshin earthquake

1923 Great Kantō earthquake and Great Hanshin earthquake have 10 things in common (in Unionpedia): Coordinated Universal Time, Honshu, Hypocenter, Japan Standard Time, Kobe, List of earthquakes in Japan, Moment magnitude scale, Peak ground acceleration, Philippine Sea Plate, Subduction.

Coordinated Universal Time

No description.

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Honshu

Honshu is the largest and most populous island of Japan, located south of Hokkaido across the Tsugaru Strait, north of Shikoku across the Inland Sea, and northeast of Kyushu across the Kanmon Straits.

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Hypocenter

A hypocenter (or hypocentre) (from ὑπόκεντρον for 'below the center') is the point of origin of an earthquake or a subsurface nuclear explosion.

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Japan Standard Time

is the standard timezone in Japan, 9 hours ahead of UTC (i.e. it is UTC+09:00).

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Kobe

is the sixth-largest city in Japan and the capital city of Hyōgo Prefecture.

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List of earthquakes in Japan

This is a list of earthquakes in Japan with either a magnitude greater than or equal to 7.0 or which caused significant damage or casualties.

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Moment magnitude scale

The moment magnitude scale (MMS; denoted as Mw or M) is one of many seismic magnitude scales used to measure the size of earthquakes.

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Peak ground acceleration

Peak ground acceleration (PGA) is equal to the maximum ground acceleration that occurred during earthquake shaking at a location.

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Philippine Sea Plate

The Philippine Sea Plate or Philippine Plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea, to the east of the Philippines.

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Subduction

Subduction is a geological process that takes place at convergent boundaries of tectonic plates where one plate moves under another and is forced or sinks due to gravity into the mantle.

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The list above answers the following questions

What 1923 Great Kantō earthquake and Great Hanshin earthquake have in common
What are the similarities between 1923 Great Kantō earthquake and Great Hanshin earthquake

1923 Great Kantō earthquake and Great Hanshin earthquake Comparison

1923 Great Kantō earthquake has 125 relations, while Great Hanshin earthquake has 85. As they have in common 10, the Jaccard index is 4.76% = 10 / (125 + 85).

References

This article shows the relationship between 1923 Great Kantō earthquake and Great Hanshin earthquake. To access each article from which the information was extracted, please visit:

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