Hakkōda Mountains

Hakkōda Mountains
八甲田山系 Hakkōda-sankei

The Hakkōda Mountains viewed from southeast.
Highest point
Peak Mount Ō
Elevation 1,584 m (5,197 ft)
Coordinates 40°39′22″N 140°52′51″E / 40.65611°N 140.88083°E / 40.65611; 140.88083Coordinates: 40°39′22″N 140°52′51″E / 40.65611°N 140.88083°E / 40.65611; 140.88083 
Geography
Country Japan
State Aomori Prefecture
Region Tōhoku
Parent range Ōu Mountains
Biome Alpine climate
Geology
Orogeny Island arc
Type of rock Volcanic

The Hakkōda Mountains (八甲田山系, Hakkōda-sankei) is a volcanic mountain range that lies to the south of Aomori city in Aomori Prefecture, Japan. The range consists of more than a dozen stratovolcanoes and lava domes arranged into two volcanic groups.[1] The Northern Hakkōda Volcanic Group emerges from the rim of an 8-km wide caldera that dates back to the Pleistocene.[1] The Southern Hakkōda Volcanic Group predates the caldera.[2]

Description

The highest peak in the range is Mount Ōdake, which can be climbed from Sukayu Onsen in about four hours. Heavy snowfall makes Hakkoda a prime destination for backcountry and mountain skiers, and there are two mountain huts for overnight trips. The lower slopes of the mountains are forested interspersed with moorland. Above 1300 meters,[3] the Alpine climate zone starts.

The Hakkōda Mountains, along with Lake Towada and the Oirase Valley make up the Towada-Hachimantai National Park.[3]

Geology

Relief map of Kita Hakkoda Volcano Group (North) & Minami Hakkoda Volcano Group (South), Hakkoda Caldera (NE)
Hakkōda Mountains as seen from the N.

The volcanic peaks are made of non-alkali mafic rock;[4] mostly andesite, dacite, and basalt.[2] Although both groups of mountains formed in the Pleistocene, the southern group is older than the northern group. The southern group is made from rock that is 700,000 to 1,700,000 years old, while the northern group is made from rock that is 13,000 to 700,000 years old.[4]

List of peaks

The following is a list of peaks and their heights:[3]

Wetlands

The Hakkōda Mountain are famous for their high-altitude wetlands:

Disaster of the Fifth Infantry Group

Memorial statue of the Hakkoda Death March, portraying Fusanosuke Gotō.

The Hakkōda Mountains incident occurred on January 23, 1902, when a group of Imperial Japanese Army soldiers marched in a blizzard on the Hakkōda Mountains en route to Tashiro Hot Spring located in the Hakkōda Mountains. The 199 deaths during a single ascent make it the world's largest mountaineering disaster in the modern history of mountain climbing.

References

  1. 1 2 3 "Hakkoda Group". Global Volcanism Program. Smithsonian National Museum of Natural History. Retrieved 2008-09-13.
  2. 1 2 "HAKKODA Caldera". Quaternary Volcanoes of Japan. National Institute of Advanced Industrial Science and Technology. 2006. Retrieved 2008-09-13.
  3. 1 2 3 Hunt, Paul (1988). "27. Hakkōda Mountains". Hiking in Japan: An Adventurer's Guide to the Mountain Trails (First ed.). Tokyo and New York: Kodansha International. pp. 172–175. ISBN 0-87011-893-5.
  4. 1 2 "Northern Tohoku". Seamless digital geological map of Japan 1:200,000. Geological Survey of Japan, AIST. May 12, 2007. Retrieved 2008-09-16.

See also

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