Jingū Seamount
Jingū Seamount, also called Jingū Guyot, is a guyot of the Hawaiian-Emperor seamount chain in the Pacific Ocean. It erupted 55 million years ago. The seamount is elongated in structure, running north–south, and has an oval shaped crater in the center, which is evidence of collapse when above sea level. The seamount was named in 1954 by Robert S. Dietz, after Japanese Empress Jingū.
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Jingū Seamount
Jingū Seamount, also called Jingū Guyot, is a guyot of the Hawaiian-Emperor seamount chain in the Pacific Ocean. It erupted 55 million years ago. The seamount is elongated in structure, running north–south, and has an oval shaped crater in the center, which is evidence of collapse when above sea level. The seamount was named in 1954 by Robert S. Dietz, after Japanese Empress Jingū.
has abstract
Jingū Seamount, also called Ji ...... after Japanese Empress Jingū.
@en
神功海山(じんぐうかいざん)とは、北太平洋の天皇海山群に位置する海山。約5500万年前に形成されたとされ、その頂上は海面下2194mである。海山名は神功皇后に由来する。
@ja
神功海底山(英語:Jingū Seamount),又稱神功海 ...... 海洋地質學家以日本神功皇后命名。山頂在海平面下2194公尺。
@zh
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Jingū Seamount, also called Ji ...... after Japanese Empress Jingū.
@en
神功海山(じんぐうかいざん)とは、北太平洋の天皇海山群に位置する海山。約5500万年前に形成されたとされ、その頂上は海面下2194mである。海山名は神功皇后に由来する。
@ja
神功海底山(英語:Jingū Seamount),又稱神功海 ...... 海洋地質學家以日本神功皇后命名。山頂在海平面下2194公尺。
@zh
label
Jingū Seamount
@en
神功海山
@ja
神功海底山
@zh