Karasawa Cirque Explained

is one of major glacial cirques in Japan, located in the Kamikochi region of Azumi, Matsumoto City, in Nagano prefecture.[1] The entire cirque and surrounding mountains are all within Chūbu-Sangaku National Park, which was designated a national park on December 4, 1934.

Outline

Karasawa Cirque lies under the peaks of Mount Hotakadake, including its highest Mount Okuhatakadake (3,190m), in the Hida Mountains or Northern Japanese Alps. Other peaks circling the glacial valley include Mount Karasawa (3,110m), Mount Kitahotakadake, and (3,106m) Maehotakadake (3,090m). Other important locations include: where, built in 1924, is located at 2983m; and a ridge, which leads to Mount Okuhatakadake.

The diameter of the cirque is about 2,000m. The floor of the cirque is 2,300m above sea level, with a difference in elevation of 900m.[2] Melting snow from the cirque helps to form the Azusa River, which flows down through the Kamikochi valley, before joining the Sai River and then the Shinano River, Japan's longest.

The area of Karasawa, Matsumoto has been designated as a by Japan Post, so it is not possible to send mail to this area from outside.[3]

Hiking and Mountaineering

Karasawa Cirque is the center for mountaineering Mount Hotakadake, and is filled with tents in summer. Climbers might also choose to stay at or . Some snow remains in summer. The cirque is also famous for the vivid colors of its autumn leaves, and is the "best autumn hike in Kamikochi".[4]

A popular, 2-day, 30 km round trip hiking route, with an 800m elevation gain, to the cirque begins at the Kamikochi Bus Terminal (1,504m), taking hikers and climbers past (approximately + 1 hour) (1,504m), + 1 hour) (1,562m), (+ 1 hour) (1,620m), (+ 1 hour) (1,780m), Karasawa Hütte (+ 2 hours) (2,300m).[5] The hike is relatively flat until Yokoo, then rises somewhat to Hontani bridge, and from there the elevation rises steeply to 2300m over a distance of 2 km.

It is also possible to hike down to Yokoo from Mount Yari (3,180) or Mount Chō (2,677m) and continue to Hontani Bridge and beyond. The most experienced climbers could traverse into the cirque, for example from Mount Yari, to Mount Nakadake, to Mount Minamidake, then along the to Mount Kitahotakadake.[6] Note that the Daikiretto gap route between Mount Yari and Mount Kitahotakadake is rated the most technically and physically challenging trail in Nagano.[7]

Karasawa Glacier

Geographer Tomoya Iozawa advocated two stages of glaciers in Japan through reading aerial photographs of Japanese Alps. The first of these is Yokoo Glacier (60 thousand years ago) and the other is Karasawa Glacier (20 thousand years ago).[8] [9] [10]

Mountain Huts

There are two major mountain huts in the cirque, Karasawa Hutte and Hut of Karasawa, and others near the surrounding peaks and rivers.

References

36.2934°N 137.6588°W

Notes and References

  1. Web site: The Karasawa Cirque, round trip from Kamikochi. 2022-08-27 . Hikes in Japan . 2020-11-13.
  2. https://www.jstage.jst.go.jp/article/jgeography1889/105/5/105_5_569/_pdf Masaki Iwafune "Rock Avalanches Occurred in the Snow-melt Season at the Karasawa Cirque in Mt. Hotaka-dake, the Japanese Alps"Journal of Geography 105(2) 569-589 1996
  3. News: 別冊(内国郵便約款第79条及び第97条関係) 交通困難地・速達取扱地域外一覧 . 2022-08-27 . . 2022-02-21.
  4. Web site: "Karasawa Cirque", the Best Autumn Hike in Kamikochi. 2022-08-27 . . 2020-11-13.
  5. Web site: The Karasawa Cirque, round trip from Kamikochi. 2022-08-27 . Hikes in Japan . 2020-11-13.
  6. Web site: Daikiretto Gap. 2022-08-27 . Hikes in Japan.
  7. Web site: Nagano Trail Guide by Grade . August 26, 2022.
  8. https://www.jstage.jst.go.jp/article/jaqua/53/6/53_275/_pdf Shuji Iwata"Turning points in the Glacial Landform Study of the Japanese Alps 第四紀研究(The Quaternary Research)53(6)p. 275─296
  9. Web site: 地球実感!長野県の地質風景/環境保全研究所. www.pref.nagano.lg.jp. 2019-01-30.
  10. https://epic.awi.de/28155/1/Polarforsch1983_1_6.pdf Ito,Vorndran"Glacial Geornorphology and Snow-Lines of Younger Quaternary around the Yari-Hotaka Mountain Range, Northern Alps, Central Japan" Polarforschung 53 (1): 75-89, 1983