Earth:Izu-Tobu
Izu-Tobu | |
---|---|
Izu-Tobu volcano field | |
Mount Ōmuro, a symbolic pyroclastic cone of the Izu-Tobu volcano field | |
Highest point | |
Coordinates | [ ⚑ ] : 34°53′59″N 139°05′52″E / 34.89972°N 139.09778°E |
Naming | |
Native name | 伊豆東部火山群 (Japanese) |
Geography | |
Geology | |
Mountain type | Pyroclastic cones |
Last eruption | July 1989 |
Izu-Tobu (伊豆東部火山群 Izu Tōbu Kazangun) 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 in 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.
Eruptions
1989 eruption
The only recorded eruption was an event on 13 July 1989. Two earthquakes, on 30 June and 9 July took, place on the Izu-Tobu Volcano. On 13 July, a seismometer recorded seismicity, a research vessel, the RV Takuyo reported hearing an explosion sound from the sea floor followed by a 30-second vibration at 18:33 pm. At 18:40 pm the crew reported that the sea domed up 500 m from the vessel, then a grey-black plume rose from the area, five more domes were reported in the next 5 minutes which caused the ship to vibrate. After that seismicity declined.
This marks the only known eruptive activity at Izu-Tobu. The next day a survey using an unmanned vessel discovered a new cone 100 metres underwater. The cone was around 450 Metres wide with a summit crater 200 m in diameter. The height of the cone above the sea floor was only 10 m in height.
The University of Tokyo monitors Izu-Tobu 24 hours a day.
Distinct cones
Image | Name | Location | Type[1][2] | Height | Eruption[1][2] | Coordinates | Comments |
---|---|---|---|---|---|---|---|
01 | omuro
Mount Ōmuro |
Itō | Cinder cone | 0580 580 m
|
004000 4 ka
|
[ ⚑ ] 34°54′11″N 139°05′40″E / 34.9031°N 139.0945°E | Lava flow formed the Jōgasaki coast. |
02
(Right)
|
komuro
Mount Komuro |
Itō | Cinder cone | 0321 321 m
|
015000 15 ka
|
[ ⚑ ] 34°56′21″N 139°07′52″E / 34.9391°N 139.131°E | |
03 | ioyama
Mount Io |
Itō | Cinder cone | 0459 459 m
|
002700 2.7 ka
|
[ ⚑ ] 34°52′18″N 139°04′46″E / 34.8717°N 139.0795°E | |
04 | togasa
Mount Tōgasa |
Izu & Higashizu |
Cinder cone | 1197 1,197 m
|
140000 14 ka - 15 ka
|
[ ⚑ ] 34°52′43″N 139°01′57″E / 34.8786°N 139.0325°E | Oldest volcano in Izu-Tobu volcano field |
05 | kawago
Kawagodaira |
Izu | Volcanic crater | 1090 approx. 1,090 m
|
003200 3.2 ka
|
[ ⚑ ] 34°51′36″N 138°58′55″E / 34.860°N 138.982°E | |
06 | maruno
Mount Maruno |
Izu | Cinder cone | 0697 697 m
|
107500 107 ka
|
[ ⚑ ] 34°54′40″N 139°01′26″E / 34.911°N 139.024°E | |
07 | sukumo
Mount Sukumo |
Izu | Cinder cone | 0581 581 m
|
132000 132 ka
|
[ ⚑ ] 35°00′18″N 139°02′13″E / 35.005°N 139.037°E | |
08 | hachikubo
Mount Hachikubo |
Izu | Cinder cone | 0674 674 m
|
017000 17 ka
|
[ ⚑ ] 34°51′43″N 138°55′44″E / 34.862°N 138.929°E | Lava flow from Mount Hachikubo formed Jōren Falls. |
09 | maruyama
|
Izu | Cinder cone | 0938 938 m
|
017000 17 ka
|
[ ⚑ ] 34°51′18″N 138°56′20″E / 34.855°N 138.939°E | |
10 | takatsuka
Mount Takatsuka |
Izunokuni | Cinder cone | 0369 369 m
|
132000 132 ka
|
[ ⚑ ] 35°00′59″N 138°58′48″E / 35.0165°N 138.98°E | Cinder cone was halved by quarrying.[citation needed] |
11 | hachino
Mount Hachino |
Kawazu | Cinder cone | 0619 619 m
|
036000 36 ka
|
[ ⚑ ] 34°47′35″N 138°58′16″E / 34.793°N 138.971°E | |
12
(Left)
|
yahazu
Mount Yahazu |
Itō | Lava dome | 0816 816 m
|
002700 2.7 ka
|
[ ⚑ ] 34°53′42″N 139°03′25″E / 34.895°N 139.057°E | |
13
(Right)
|
anano
Mount Anano |
Itō | Lava dome | 0660 660 m
|
002700 2.7 ka
|
[ ⚑ ] 34°54′00″N 139°03′11″E / 34.9°N 139.053°E | |
14 | iwano
Mount Iwano |
Izu | Lava dome | 0602 602 m
|
002700 2.7 ka
|
[ ⚑ ] 34°54′47″N 139°02′20″E / 34.913°N 139.039°E | |
15 | ippeki
Ippeki lake |
Itō | Maar | 0185
Surface elevation |
103500 103.5 ka
|
[ ⚑ ] 34°55′48″N 139°06′18″E / 34.93°N 139.105°E | |
16 | jogasaki
Jōgasaki coast |
Itō | Lava flow | -
|
004000 4 ka
|
[ ⚑ ] 34°53′24″N 139°08′17″E / 34.89°N 139.138°E | This coast was mostly formed by lava flow from Mount Ōmuro. |
17 | teishi
Teishi knoll |
Sagami Sea (off Itō) | Volcanic crater | ||||
001989 13 July 1989
|
[ ⚑ ] 34°59′06″N 139°07′08″E / 34.985°N 139.118889°E | Youngest volcano in Izu-Tobu volcano field. Eruption video by Japan Coast Guard |
See also
- List of volcanoes in Japan
- List of mountains in Japan
References
External links
- Izu-Tobu Volcanoes – Japan Meteorological Agency (in Japanese)
- "Izu-Tobu Volcanoes : National catalogue of the active volcanoes in Japan". http://www.data.jma.go.jp/svd/vois/data/tokyo/STOCK/souran_eng/volcanoes/057_izu-tobu_volcanoes.pdf. – Japan Meteorological Agency
- Izu Tobu Volcano Group – Geological Survey of Japan
- Eruptive history of the Higashi Izu monogenetic volcano field – Shizuoka University
Original source: https://en.wikipedia.org/wiki/Izu-Tobu.
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