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Japan Trench

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Japan Trench 

a submarine depression in the western part of the Pacific Ocean, along the eastern edge of Honshu. The Japan Trench is about 1,000 km long and reaches a maximum depth of 8,412 m. Its cross section is V-shaped: the width of the trench within the isobath ranges from 7 km to about 60 km, while on the bottom it ranges from 1.8 to 36 km. There are numerous earthquake epicenters confined to the sides and bottom of the trench.



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The Pseudoliparis amblystomopsis were found in the Pacific Ocean's Japan Trench.
The main cause appears to have been a collision of two chains of seabed mountains into the Japan Trench on the ocean floor about 200 kms (120 miles) east of modern-day Tokyo.
The main cause appears to have been a collision of two chains of seabed mountains into the Japan Trench on the ocean floor about 200 kms (120 miles) east of modern-day Tokyo.
 
 
 
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