Translator Reviews ( Japanese → English )

Japanese

実は富士山は3階建です。一体、どういう事なのか？
今から10万年以上前、いまの伊豆半島は現在のハワイ辺りにありました。それが段々と北に移動してきて日本の本州にぶつかり、盛り上がって山が出来ました。その時に出来た山が富士山の1階になる小御岳です。その後、今から10万年～1万年以上前に、小御岳の脇で何度も大きな噴火がありました。繰り返し噴出した溶岩は冷えて固まり積み重なっていきました。このようにして出来たのが今の富士山の原型で2階部分となる古富士です。

English

Actually, Mt. Fuji has three stories. What is the meaning of it?
About 10,000 years ago, the present Izu peninsula was located around present Hawaii. Then, it had moved toward North, hit the main island of Japan(Honshu), rose the ground, and conposed mountain. This became Komitake which was first story of Mt. Fuji.
After that, more than 10,000 to 100,000 years ago, there were lots of big eruptions besides Komitake. Because of the successive eruptions, the lava had gotten cold and been accumulated.
In this way, the basis of present Mt. Fuji and the second story called old Mt. Fuji was formed.

Reviews ( 1 )

katrina_z rated this translation result as ★★★ 12 Aug 2013 at 02:02

original
Actually, Mt. Fuji has three stories. What is the meaning of it?
About 10,000 years ago, the present Izu peninsula was located around present Hawaii. Then, it had moved toward North, hit the main island of Japan(Honshu), rose the ground, and conposed mountain. This became Komitake which was first story of Mt. Fuji.
After that, more than 10,000 to 100,000 years ago, there were lots of big eruptions besides Komitake. Because of the successive eruptions, the lava had gotten cold and been accumulated.
In this way, the basis of present Mt. Fuji and the second story called old Mt. Fuji was formed.

corrected
Actually, Mt. Fuji has three stories. What is the meaning of it?
About 100,000 years ago, the present Izu peninsula was located around present Hawaii. Then, it had moved toward the north, hit the main island of Japan (Honshu), pushed the ground up, and created a mountain. This became Komitake which was the first story of Mt. Fuji.
After that, more than 100,000 to 10,000 years ago, there were lots of big eruptions besides Komitake. The lava that came from these successive eruptions cooled and accumulated.
In this way, the basis of present Mt. Fuji and the second story called old Mt. Fuji was formed.