Lake Mashū Explained

Lake Mashū
摩周湖
Coords:43.5833°N 175°W
Pushpin Map:Japan
Inflow:two streams
Outflow:seepage
Catchment:32.4km2
Basin Countries:Japan
Length:6km (04miles)
Area:19km2
Depth:137.5m (451.1feet)
Max-Depth:211.5m (693.9feet)
Volume:2.86km3
Shore:19.8km (12.3miles)
Elevation:351m (1,152feet)
Islands:Kamuishu Island
Cities:none
Frozen:December to April

(Ainu: Kamuy-to) is an endorheic crater lake formed in the caldera of a potentially active volcano. It is located in Akan Mashu National Park on the island of Hokkaido, Japan. It has been called the clearest lake in the world.

Hydrology

Lake Mashū is surrounded by steep crater walls 200m (700feet) high. It has no significant inlets[1] and no outlet. The lake is one of the clearest in the world and one of the deepest in Japan.[2] On August 1, 1931, the transparency of the water was measured at 41.6m (136.5feet). Around the same time Lake Baikal was measured 40.5m (132.9feet). This is the basis for the lake's claim to be the clearest in the world. Since the 1950s the transparency has tended to range between 20mand30mm (70feetand100feetm).[3] The loss in transparency is probably due to the introduction of sockeye salmon and rainbow trout into the lake and landslides.[4] At the same time, the clarity of Lake Baikal has not been measured.[5]

In summer, the surface of Lake Mashū is often obscured by fog. There is usually fog covering around the lake for about 100 days of the year. This has given the lake a reputation for mysteriousness.[6] A local legend says that if you can see the surface of the lake, you will have bad luck.

Origin of the name

The origin of Lake Mashū's name is unclear. The lake's original Ainu name was Kintan-kamuy-to or lake of the mountain god. Ainu language researcher Nagata Housei proposed that that the Japanese name originated from the Ainu Mas-un-to or lake of the gulls.[7] This was then rendered as by the Japanese. Over time, however, the Japanese began to refer to the lake by the Japanese reading for the neighboring peak, .[8] The kanji for this peak translate roughly as scrubbed area mountain. The Ainu name for this peak, by which it is commonly known today, is Kamuinupuri or mountain of the gods. The lake also retains its Ainu name in a shortened form, as Kamuyto or lake of the gods.

Volcanic caldera

Mashū formed less than 32,000 years ago. The caldera is the remains of a stratovolcano, which is actually a parasitic cone of the larger Lake Kussharo caldera. The eruption that created the current caldera occurred around 7,000 years ago. The last eruption was a plinian eruption about 2,000 years ago that dropped pumice over the region.

Mashū volcano is rated with a Volcanic Explosivity Index of 6, the third highest among large volcanoes.[9]

Two volcanoes have grown out of the Mashū caldera. Kamuishu Island, a lava dome which rises from the middle of the lake, is one. The other is Mount Kamui, a stratovolcano with lava dome, which forms the highest point on the eastern shore. A third volcano neighbors Kamuinupuri. It is Mount Nishibetsu. Mount Nishibetsu probably predates the caldera.

The main rock type of the volcanoes is andesite and dacite. The rock is non-alkali pyroclastic flow or mafic rock, dating from the Late Pleistocene to the Holocene. Some rock around the Mashū crater and Mount Nishibetsu is older still, dating from the Middle Pleistocene.[10]

The following table lists the eruptions of the Mashū volcano and Kamuinupuri.[11]

VolcanoDate of eruptionDating techniqueVEITephra volumeType
Mashū 7400 BC ± 200 yearsCorrected radiocarbon4440000000m2Explosive eruption
Mashū 6600 BC ± 50 yearsCorrected radiocarbon611000000000m2Explosive eruption of the central vent with pyroclastic flow and caldera collapse
Mount Kamui2750 BC ± 100 yearsCorrected radiocarbonExplosive eruption of a flank vent
Mount Kamui1400 BC ± 100 yearsCorrected radiocarbonExplosive eruption of a flank vent
Mount Kamui100 BC ± 500 yearsTephrochronologyExplosive eruption
Mount Kamui300 AD ± 75 yearsCorrected radiocarbonExplosive eruption
Mount Kamui970 AD ± 100 yearsUncorrected radiocarbon51000000000m2Explosive eruption of a flank vent and caldera collapse

Flora and fauna

The lake is inhabited by phytoplankton and zooplankton.

Sockeye salmon and rainbow trout have been introduced to the lake.

On the slopes around and above the lake grow a mixture of evergreen forest with Picea jezoensis and Abies sachalinensis and birch forest with Betula ermanii.

Economy

The Mashu-dake Hiking Course is a trail that goes along the crater rim and to the top of Mount Mashū. The trail leads through forest and grassland for about seven kilometers and takes about 2.5 to 3 hours to hike one way. There are no settlements along the shores of the lake. Access to the lakeshore itself is prohibited by the Ministry of the Environment (Japan). Visitors may only view the lake from the designated observation towers.

In popular culture

Sendoff Spring in Pokémon Diamond and Pearl and Pokémon Platinum is based on this lake as the Sinnoh region is a fictionalized version of Hokkaido.

See also

External links

Notes and References

  1. Web site: MASHU-KO (LAKE MASHU). World Lakes Database. International Lake Environment Committee. 2008-10-15. dead. https://web.archive.org/web/20120229165323/http://www.ilec.or.jp/database/asi/asi-22.html. 2012-02-29.
  2. Book: Bisignani, J. D.. Japan Handbook. Taran March. Moon Publications, Inc.. Chico, California. December 1993. Second. 805–807. Doto~Eastern Hokkaido. 0-918373-70-0. https://archive.org/details/japanhandbook0000bisi/page/805.
  3. September 2004. GEMS/Water 摩周湖モニタリングデータブック. Cger's Supercomputer Monograph Report . Center for Global Environmental Research. 1341-4356. Japanese.
  4. NHK World HD Channel
  5. Web site: Lake Mashu. Highlights: Eastern Hokkaido. Akan Tourism Association & Community Development Promotion Organization . 2008-10-15.
  6. Book: Hunt, Paul . Hiking in Japan: An Adventurer's Guide to the Mountain Trails . Kodansha International . 1988 . 0-87011-893-5 . First . New York and Tokyo . 195–200 . 32. Climbing an Active Volcano: Meakan-dake.
  7. Web site: 2024-05-31 . Lake Mashu DATA (摩周湖DATA) . https://web.archive.org/web/20240414112030/https://www.masyuko.or.jp/enjoy/sightseeing/spot/mashu_2 . 2024-04-14 . 2024-05-31 . masyuko.or.jp.
  8. ,, page 128, (in Japanese).
  9. Web site: Large Volcano Explocivity Index . 2011-03-08.
  10. Web site: Hokkaido. 2007. Seamless Digital Geological Map of Japan. Geological Survey of Japan, AIST. 2010-09-28. 2013-01-06. https://web.archive.org/web/20130106003942/http://riodb02.ibase.aist.go.jp/db084/kihon/hokkaido_e.xml. dead.
  11. 285081. Mashu: Eruptive History. Eruptions. 2020-03-23.