Geology of Japan
Encyclopedia
The islands of Japan
are primarily the result of several large oceanic movements occurring over hundreds of millions of years from the mid-Silurian
to the Pleistocene
as a result of the subduction
of the Philippine Sea Plate beneath the continental Amurian Plate
and Okinawa Plate
to the south, and subduction of the Pacific Plate
under the Okhotsk Plate
to the north.
Japan was originally attached to the eastern coast of the Eurasia
n continent. The subducting plates, being deeper than the Eurasian plate, pulled Japan eastward, opening the Sea of Japan
around 15 million years ago. The Strait of Tartary
and the Korea Strait
opened much later.
Japan is situated in a volcanic
zone on the Pacific Ring of Fire
. Frequent low intensity earth tremors and occasional volcanic activity are felt throughout the islands. Destructive earthquake
s, often resulting in tsunami
s, occur several times a century. The most recent major quakes include the 2011 Tōhoku earthquake and tsunami
, the 2004 Chūetsu earthquake
and the Great Hanshin Earthquake
of 1995. Hot springs
are numerous and have been developed as resorts.
Japan
Japan is an island nation in East Asia. Located in the Pacific Ocean, it lies to the east of the Sea of Japan, China, North Korea, South Korea and Russia, stretching from the Sea of Okhotsk in the north to the East China Sea and Taiwan in the south...
are primarily the result of several large oceanic movements occurring over hundreds of millions of years from the mid-Silurian
Silurian
The Silurian is a geologic period and system that extends from the end of the Ordovician Period, about 443.7 ± 1.5 Mya , to the beginning of the Devonian Period, about 416.0 ± 2.8 Mya . As with other geologic periods, the rock beds that define the period's start and end are well identified, but the...
to the Pleistocene
Pleistocene
The Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....
as a result of the subduction
Subduction
In geology, subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate, sinking into the Earth's mantle, as the plates converge. These 3D regions of mantle downwellings are known as "Subduction Zones"...
of the Philippine Sea Plate beneath the continental Amurian Plate
Amurian Plate
The Amurian Plate is a proposed continental tectonic plate covering Manchuria, the Korean Peninsula, Western Japan, and Primorsky Krai...
and Okinawa Plate
Okinawa Plate
The Okinawa Plate is a long narrow tectonic plate stretching from the northern end of Taiwan to the southern tip of the island of Kyūshū. To the east lies the Ryukyu Trench and the Pacific Plate. It is separated from the Yangtze Plate by a rift that forms the Okinawa Trough which is a Back arc...
to the south, and subduction of the Pacific Plate
Pacific Plate
The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At 103 million square kilometres, it is the largest tectonic plate....
under the Okhotsk Plate
Okhotsk Plate
The Okhotsk Plate is a tectonic plate covering the Sea of Okhotsk, the Kamchatka Peninsula, Sakhalin Island and Tōhoku and Hokkaidō in Japan. It was formerly considered a part of the North American Plate, but recent studies indicate that it is an independent plate, bounded on the north by the...
to the north.
Japan was originally attached to the eastern coast of the Eurasia
Eurasia
Eurasia is a continent or supercontinent comprising the traditional continents of Europe and Asia ; covering about 52,990,000 km2 or about 10.6% of the Earth's surface located primarily in the eastern and northern hemispheres...
n continent. The subducting plates, being deeper than the Eurasian plate, pulled Japan eastward, opening the Sea of Japan
Sea of Japan
The Sea of Japan is a marginal sea of the western Pacific Ocean, between the Asian mainland, the Japanese archipelago and Sakhalin. It is bordered by Japan, North Korea, Russia and South Korea. Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure from the Pacific...
around 15 million years ago. The Strait of Tartary
Strait of Tartary
Strait of Tartary is a strait in the Pacific Ocean dividing the Russian island of Sakhalin from mainland Asia , connecting the Sea of Okhotsk on the north with...
and the Korea Strait
Korea Strait
The Korea Strait is a sea passage between South Korea and Japan, connecting the East China Sea and the Sea of Japan in the northwest Pacific Ocean...
opened much later.
Japan is situated in a volcanic
Volcano
2. Bedrock3. Conduit 4. Base5. Sill6. Dike7. Layers of ash emitted by the volcano8. Flank| 9. Layers of lava emitted by the volcano10. Throat11. Parasitic cone12. Lava flow13. Vent14. Crater15...
zone on the Pacific Ring of Fire
Pacific Ring of Fire
The Pacific Ring of Fire is an area where large numbers of earthquakes and volcanic eruptions occur in the basin of the Pacific Ocean. In a horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and/or plate movements...
. Frequent low intensity earth tremors and occasional volcanic activity are felt throughout the islands. Destructive earthquake
Earthquake
An earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time...
s, often resulting in tsunami
Tsunami
A tsunami is a series of water waves caused by the displacement of a large volume of a body of water, typically an ocean or a large lake...
s, occur several times a century. The most recent major quakes include the 2011 Tōhoku earthquake and tsunami
2011 Tōhoku earthquake and tsunami
The 2011 earthquake off the Pacific coast of Tohoku, also known as the 2011 Tohoku earthquake, or the Great East Japan Earthquake, was a magnitude 9.0 undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST on Friday, 11 March 2011, with the epicenter approximately east...
, the 2004 Chūetsu earthquake
2004 Chuetsu earthquake
The occurred at 5:56 p.m. on Saturday, October 23, 2004 . The Japan Meteorological Agency has named it the Heisei 16 Niigata Prefecture Chuetsu Earthquake or The Mid Niigata Prefecture Earthquake of 2004...
and the Great Hanshin Earthquake
Great Hanshin earthquake
The Great Hanshin earthquake, or Kobe earthquake, was an earthquake that occurred on Tuesday, January 17, 1995, at 05:46 JST in the southern part of Hyōgo Prefecture, Japan. It measured 6.8 on the moment magnitude scale , and Mj7.3 on JMA magnitude scale. The tremors lasted for approximately 20...
of 1995. Hot springs
Onsen
An is a term for hot springs in the Japanese language, though the term is often used to describe the bathing facilities and inns around the hot springs. As a volcanically active country, Japan has thousands of onsen scattered along its length and breadth...
are numerous and have been developed as resorts.
See also
- Seismicity in Japan
- List of earthquakes in Japan
- List of volcanoes in Japan
- Category: Japanese geologists
External links
- Geological Survey of Japan
- National Archives of JapanNational Archives of JapanThe preserve Japanese government documents and historical records and make them available to the public. Although Japan's reverence for its unique history and art is well documented and illustrated by collections of art and documents, there is almost no archivist tradition...
: Tatoroyama no ki, survey of limestone cave in Mount Tatoro in Kozuke Province, 1837 (Tenpo 8).