Mount Kaimon


Kaimondake, or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small complex central lava dome – 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 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as "the Fuji of Satsuma". It is one of the 100 Famous Japanese Mountains.

Geography

Mt. Kaimon is located in the south of Kagoshima prefecture, Kyushu and is an important reference point for marine traffic because it is the southernmost prominence of the Satsuma Peninsula. This is one entrance marker to Kinko Bay complimentary to the Ōsumi Peninsula. Together with Mt. Noma and Mt. Kinpo, it is used by marine traffic.

Geology

Part of the Ibusuki volcanic field, Mt. Kaimon defines the eastern margin of the old Ata Caldera. The total eruptive volume of tephra has been and of lava.
There is a sea scarp which is 7.8 km wide and 9.3 km 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 from the eruption at the end of the 7th century is called ao-kora. The sedimentary layer of ejecta by the eruption at the end of the 7th century is called murasaki-kora. These layers are a clue to know the changes in life in this era. It has become clear that a village was isolated by a large eruption with change in life style in the latter part of the 9th century.

Eruptive history

Mount Kaimon began volcanic activity about 4,000 years ago. From 3,000 years up to 885 years ago, large eruptions occurred 9 times and eruptions resulting in large amounts of lava occurred 10 times making twelve major eruptions to date.
The two large eruptions in the historic written record are in 874 CE and 885 CE
The complex layered central dome consists of a scoria cone topped by lava flows and ultimately a lava dome which was penetrated by a plug. However the explosion crater at the top was last enlarged by the 885 CE eruption.
DateDRETephraLavaComment
885 CEKm-Nn tephra pyroclastic flow to the east
874 CE–Km-Jo tephra
500 CEKm-11
200 CE–Km-10
0 CE–Km-9
– 100 BCEKm-8
– 300 BCEKm-7
– 500 BCE–Km-6
– 900 BCEKm-5 under sea lava flows
– 1200 BCE–Km-4 large tephra fall to north west
– 1400 BCE–Km-3
– 1600 BCE–Km-2
– 2000 BCEKm-1

Transition of height

In 1895, the official height of Mt. Kaimon was from a second triangulation point which was at the summit of the mountain, but this was updated to by the Geospatial Information Authority of Japan in July 2001, because climbers pointed out that the height of the rocks on the top of the mountain were higher than the triangulation point.

Climbing

The spiral-shaped hiking trail climb of Mt. Kaimon takes about 3 hours. Mt. Kaimon is considerably lower than most of the mountains on the 100 famous Japanese Mountains list but as climbing starts from close to sea level there is an ascent of. Mt. Kaimon is a single peak but with summit rocky outcrops that allow views on all sides, such as Lake Ikeda to the north and the Pacific Ocean to the south.

Tourism