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・ Izuru Narushima
・ Izuru Takeuchi
・ Izusan Jinja
・ Izushi Castle
・ Izushi District, Hyōgo
・ Izushi jinja
・ Izu-Atagawa Station
・ Izu-Bonin-Mariana Arc
・ Izu-Hokkawa Station
・ Izu-Inatori Station
・ Izu-Kōgen Station
・ Izu-Nagaoka Station
・ Izu-Nitta Station
・ Izu-Ogasawara Trench
・ Izu-Taga Station
Izu-Tobu
・ Izu-Ōkawa Station
・ Izuchukwu Aniche
・ Izudin Dervic
・ Izudin Čavrković
・ Izue Station
・ Izuhakone 1100 series
・ Izuhakone Railway
・ Izuhakone Railway Sunzu Line
・ Izuka
・ Izuki Formation
・ Izuki Kogyoku
・ Izuki Tanaka
・ Izukirudo
・ Izukyū Corporation


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Izu-Tobu : ウィキペディア英語版
Izu-Tobu

is a large, dominantly basaltic range of volcanoes on the east side of the Izu Peninsula which lies on the Pacific coast of the island of Honshu, Japan. The field covers a total area of 400 km2. The only recorded activity was a submarine phreatic eruption, between the city of Ito and Hatsushima island, that lasted for just 10 minutes in 1989. Ito, home to 74,000 people, is known for its hot springs.
== Morphology ==
The field covers the east side of the Izu Peninsula. It consists of several small stratovolcanoes (mostly Pleistocene in age) and overlapping pyroclastic cones, which covers 400 km2 in area. There are 70 young monogenetic volcanoes on land. Kawagodaira maar, which is about 3,000 years old, produced a large Holocene eruption that sent pyroclastic flows over a wide area.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Izu-Tobu」の詳細全文を読む



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