Mount Kaimon: Difference between revisions

Coordinates: 31°10′48″N 130°31′42″E / 31.18000°N 130.52833°E / 31.18000; 130.52833
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{{Nihongo|'''Kaimondake'''|開聞岳|Kaimondake, Kaimon-dake}}, or '''Mount Kaimon''', is an undissected [[volcano]] – consisting of a basal stratovolcano and a small central volcano, part of the Ibusuki field – which rises to a height of 924 metres above sea level near the city of [[Ibusuki, Kagoshima|Ibusuki]] in southern [[Kyūshū]], [[Japan]]. The last eruption occurred in the year 885.Because the shape of mountain is corn, Mt. Kaimon is sometimes referred to as"the Fuji of [[Satsuma Province|Satsuma]]".
{{Nihongo|'''Kaimondake'''|開聞岳|Kaimondake, Kaimon-dake}}, or '''Mount Kaimon''', is an undissected [[volcano]] – consisting of a basal stratovolcano and a small central volcano, part of the Ibusuki field – which rises to a height of 924 metres above sea level near the city of [[Ibusuki, Kagoshima|Ibusuki]] in southern [[Kyūshū]], [[Japan]]. The last eruption occurred in the year 885. Because of its conic shape, Mt. Kaimon is sometimes referred to as "the Fuji of [[Satsuma Province|Satsuma]]".


== History ==
== History ==

Revision as of 14:37, 26 August 2022

Kaimondake
開聞岳
Highest point
Elevation924 m (3,031 ft)
Coordinates31°10′48″N 130°31′42″E / 31.18000°N 130.52833°E / 31.18000; 130.52833
Geography
Kaimondake is located in Japan
Kaimondake
Kaimondake
Geology
Mountain typestratovolcano
Last eruption885[1]

Kaimondake (開聞岳, Kaimondake, Kaimon-dake), or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small central volcano, part of the Ibusuki field – which rises to a height of 924 metres above sea level near the city of Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885. Because of its conic shape, Mt. Kaimon is sometimes referred to as "the Fuji of Satsuma".

History

Mt. Kaimon began volcanic activity 4000 years ago. For 3,000 years up to 885 years, the big eruptions occurred 9 times and the eruption that a lot of magma was erupted occurred 10 times.

There is a sea scarp which is 7.8km wide and 9.3km long, the shape is similar to a horseshoe in the seabed at the southern foot of the mountain. There is a lot of sediment at the foot of the mountain due to submarine landslides. It was found that there is a sea scarp underground on the south side of the mountain and it was caused by pressure from a submarine landslide before Mt. Kaimon was formed.

The sedimentary layer of ejecta by the eruption at the end of the 7th century is called ao-kora (ao means blue and kora is soil consisting of volcanic ash found in the southern part of the Satsuma Peninsula), The sedimentary layer of ejecta by the eruption at the end of the 7th century is called murasaki-kora (Murasaki means purple). These layers are a clue to know the changes in life in this era. It has become clear that village was isolated by big eruption and change in life in the latter part of the 9th century.

Geography

Mt. Kaimon is important symbol of marine traffic because it is in the southernmost of Satsuma Peninsula which is located in the south of Kagoshima prefecture and forms Kinko Bay (Kagoshima Bay) with Ōsumi Peninsula, just the south of Kyushu. Together with Mt. Noma and Mt. Kinpo, it also forms part of the three mountains of Satsuma, which are also used by marine traffic.

Transition of height

In 1895, the height of Mt. Kaimon was 922.23 meters from a second triangulation point which is at the summit of the mountain but the official height was fixed 924 meters by Geospatial Information Authority of Japan in 2001, July because some climbers pointed out that the height of the rocks on the top of the mountain were higher than the triangulation point.[2]

Climbing

There is spiral-shaped hiking trail, and you can climb Mt. Kaimon in about 3 hours. Mt. Kaimon is considerably lower than most of the mountains on the 100 famous Japanese Mountains list but climbing starts from around sea level going up more than 900 meters. Mt. Kaimon is a single peak and near the summit rocky outcrops give views on all sides, such as Lake Ikeda to the north and the Pacific Ocean to the south.

Tourism

  • Kaimon Sanroku Nature Park-There are Tokara horse at the base of the mountain. [3]
  • Kaimon Sanroku Fureai Park- There are log houses, camp sites and so on. [4]
  • Lake Ikeda- It is said that a mystery creature “Issie” live there. There are beautiful canola flowers in January. [5]
  • Bohi Park-This is the park which console the people who were killed in the Pacific War in Philippines.

See also

References

  1. ^ "Ata: Eruptive History". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-24.
  2. ^ 「開聞岳少しだけ高かった/新標高2メートル伸び924メートル=最高地点移動、登山者が指摘」南日本新聞2001年8月17日朝刊27面
  3. ^ https://www.ibusuki.or.jp/tourism/play/post-39/開聞山麓自然公園 | いぶすき観光ネット-Retrieved 2022-05-31
  4. ^ https://www.ibusuki.or.jp/tourism/play/kaimonpark/かいもん山麓ふれあい公園 | いぶすき観光ネット-Retrieved 2022-05-31
  5. ^ https://www.kagoshima-kankou.com/guide/10670池田湖 | 観光スポット | 【公式】鹿児島県観光サイト かごしまの旅-Retrieved 2022-05-31

External links