Mount Iwate

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Mount Iwate
岩手山
Mt. Iwate and Morioka.jpg
Mount Iwate from the city of Morioka
Highest point
Elevation 2,038 m (6,686 ft) [1]
Prominence 1,745 m (5,725 ft) [1]
Listing 100 Famous Mountains of Japan
Ultra
Coordinates 39°51′12″N 141°00′03″E / 39.85333°N 141.00083°E / 39.85333; 141.00083Coordinates: 39°51′12″N 141°00′03″E / 39.85333°N 141.00083°E / 39.85333; 141.00083
Geography
Mount Iwate is located in Iwate Prefecture
Mount Iwate
Mount Iwate
Mount Iwate
Mount Iwate is located in Japan
Mount Iwate
Mount Iwate
Mount Iwate
Location Iwate Prefecture, Japan
Parent range Ōu Mountains
Geology
Mountain type Stratovolcano complex
Last eruption July 1919

Mount Iwate (岩手山, Iwate-san) is a stratovolcano complex in the Ōu Mountains of western Iwate Prefecture, in the Tōhoku region of northern Honshū, Japan. With an elevation of 2,038 metres (6,686 ft), it is the highest in Iwate Prefecture. It is included as one of the 100 famous mountains in Japan, a book composed in 1964 by mountaineer and author Kyūya Fukada.[2] The mountain is on the borders of the municipalities of Hachimantai, Takizawa, and Shizukuishi, west of the prefectural capital of Morioka. Much of the mountain is within the borders of the Towada-Hachimantai National Park.[3][4][5] The mountain is also referred to as the "Nanbu Fuji" for its resemblance to Mount Fuji.

Geology[edit]

Aerial photographs of Mount Iwate from the NNW
Relief Map

Mount Iwate consists of a younger eastern symmetrical stratovolcano (Higashi-Iwate, "East Iwate") overlapping an older western stratovolcano (Nishi-Iwate, "West Iwate") which has collapsed to form a caldera.[6] Nishi-Iwate was formed approximately 700,000 years ago, and forms two-thirds of the mountain body. Nishi-Iwate was a later (300,000 years ago) parasitic volcano, which now forms the summit of the mountain. The oval-shaped, 1.8 x 3 km caldera of Nishi-Iwate has a 0.5 km wide crater, partially filled by a crater lake called Lake Onawashiro. Several somma including Yakushidake, the largest, surround the more recent Higashi Iwate crater rim.

During the historical period, Mount Iwate erupted in 1686-1687 with a pyroclastic surge; however, the eruption of 1732 was much larger and resulted in a substantial lava flow on the northeast slopes of the mountain. This four-kilometre long lava flow ("Yakebashiri Lava Flow") has been designated a Natural Monument by the Japanese government. Mount Iwate has largely been quiet since 1732, with a small emission of steam and ash in 1919 and a series of volcanic earthquakes from 1998 to 2003.

See also[edit]

References[edit]

  1. ^ a b c "Japan Ultra-Prominences". Peaklist.org. Retrieved 2015-01-01. 
  2. ^ Hyakumeizan, Hiking Japan!. Japan Gazetteer. Accessed June 27, 2008.
  3. ^ "Introducing places of interest: Towada-Hachimantai National Park". Ministry of the Environment. Retrieved 29 February 2012. 
  4. ^ "Towada-Hachimantai National Park". Natural Parks Foundation. Retrieved 29 February 2012. 
  5. ^ Sutherland, Mary; Britton, Dorothy (1995). National Parks of Japan. Kodansha. pp. 48–50. ISBN 4-7700-1971-8. 
  6. ^ "Iwate". Global Volcanism Program. Smithsonian Institution. 

External links[edit]