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Lake Mashū

Coordinates: 43°35′N 144°31′E / 43.583°N 144.517°E / 43.583; 144.517
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Lake Mashū
摩周湖
Lake Mashū, Japan, during winter
Lake Mashū 摩周湖 is located in Japan
Lake Mashū 摩周湖
Lake Mashū
摩周湖
LocationTeshikaga, Kushiro Subprefecture, Hokkaido, Japan
Coordinates43°35′N 144°31′E / 43.583°N 144.517°E / 43.583; 144.517
Typecrater lake, endorheic
Primary inflowstwo streams
Primary outflowsseepage
Catchment area32.4 km2 (12.5 sq mi)
Basin countriesJapan
Max. length6 km (3.7 mi)
Surface area19 km2 (4,700 acres)
Average depth137.5 m (451 ft)
Max. depth211.5 m (694 ft)
Water volume2.86 km3 (0.69 cu mi)
Shore length119.8 km (12.3 mi)
Surface elevation351 m (1,152 ft)
FrozenDecember to April
IslandsKamuishu Island
Settlementsnone
1 Shore length is not a well-defined measure.

Lake Mashū (摩周湖, Mashū-ko) (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

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View from Viewing Platform No. 1 (July 2008)
Landsat image of the lake (1999)
Map of Hokkaido showing location of Lake Mashū and Mount Kamui

Lake Mashū is surrounded by steep crater walls 200 metres (660 ft) 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 41.6 metres (136 ft). Around the same time Lake Baikal was measured 40.5 metres (133 ft). This is the basis for the lake's claim to be the clearest in the world.[1] Since the 1950s the transparency has tended to range between 20 and 30 metres (66 and 98 ft).[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 a person can see the surface of the lake, they will have bad luck.[5]

Origin of the name

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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 Lake Mashin (魔神湖, Mashin-ko) by the Japanese. Over time, however, the Japanese began to refer to the lake by the Japanese reading for the neighboring peak, Mount Mashū (摩周岳, Mashū-dake).[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

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Relief map of Kussharo Caldera (left) & Mashu Caldera (right)

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.[6] 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]

Volcano Date of eruption Dating technique VEI Tephra volume Type
Mashū 7400 BC ± 200 years Corrected radiocarbon 4 440,000,000 cubic metres (0.11 cu mi) Explosive eruption
Mashū 6600 BC ± 50 years Corrected radiocarbon 6 11,000,000,000 cubic metres (2.6 cu mi) Explosive eruption of the central vent with pyroclastic flow and caldera collapse
Mount Kamui 2750 BC ± 100 years Corrected radiocarbon Explosive eruption of a flank vent
Mount Kamui 1400 BC ± 100 years Corrected radiocarbon Explosive eruption of a flank vent
Mount Kamui 100 BC ± 500 years Tephrochronology Explosive eruption
Mount Kamui 300 AD ± 75 years Corrected radiocarbon Explosive eruption
Mount Kamui 970 AD ± 100 years Uncorrected radiocarbon 5 1,000,000,000 cubic metres (0.24 cu mi) Explosive eruption of a flank vent and caldera collapse

Flora and fauna

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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

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Lake Mashū in the winter

The Mashu-dake Hiking Course is a trail that goes along the crater rim and to the top of Mount Mashū.[2] 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.[1]

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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

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References

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  1. ^ a b c "MASHU-KO (LAKE MASHU)". World Lakes Database. International Lake Environment Committee. Archived from the original on 2012-02-29. Retrieved 2008-10-15.
  2. ^ a b Bisignani, J. D. (December 1993). "Doto~Eastern Hokkaido". In Taran March (ed.). Japan Handbook (Second ed.). Chico, California: Moon Publications, Inc. pp. 805–807. ISBN 0-918373-70-0.
  3. ^ "GEMS/Water 摩周湖モニタリングデータブック" (PDF). Cger's Supercomputer Monograph Report (in Japanese). Center for Global Environmental Research. September 2004. ISSN 1341-4356.
  4. ^ NHK World HD Channel
  5. ^ a b "Lake Mashu". Highlights: Eastern Hokkaido. Akan Tourism Association & Community Development Promotion Organization. Retrieved 2008-10-15.
  6. ^ a b Hunt, Paul (1988). "32. Climbing an Active Volcano: Meakan-dake". Hiking in Japan: An Adventurer's Guide to the Mountain Trails (First ed.). New York and Tokyo: Kodansha International. pp. 195–200. ISBN 0-87011-893-5.
  7. ^ "Lake Mashu DATA (摩周湖DATA)". masyuko.or.jp. 2024-05-31. Archived from the original on 2024-04-14. Retrieved 2024-05-31.
  8. ^ Akagi Sanpei (赤木 三兵), Journey of Hokkaidō Place Names—Notes on Ainu Language Place Names (北海道 地名の旅—アイヌ語地名解, Hokkaidō Chimei no Tabi — Ainugo Chimei Kai), page 128, (in Japanese).
  9. ^ "Large Volcano Explocivity Index". Retrieved 2011-03-08.
  10. ^ "Hokkaido". Seamless Digital Geological Map of Japan. Geological Survey of Japan, AIST. 2007. Archived from the original on 2013-01-06. Retrieved 2010-09-28.
  11. ^ "Mashu: Eruptive History". Global Volcanism Program. Smithsonian Institution. Retrieved 2020-03-23.
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