Lake Mashū
Template:Short description Template:Infobox body of water Template:Nihongo (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 Template:Convert high. It has no significant inlets<ref name="ILEC">Template:Cite web</ref> and no outlet. The lake is one of the clearest in the world and one of the deepest in Japan.<ref name="Bisignani">Template:Cite book</ref> On August 1, 1931, the transparency of the water was measured at Template:Convert. Around the same time Lake Baikal was measured Template:Convert. This is the basis for the lake's claim to be the clearest in the world.<ref name="ILEC" /> Since the 1950s the transparency has tended to range between Template:Convert.<ref name="GEMS">Template:Cite journal</ref> The loss in transparency is probably due to the introduction of sockeye salmon and rainbow trout into the lake and landslides.<ref name="Akan NHK World HD Channel">NHK World HD Channel</ref> At the same time, the clarity of Lake Baikal has not been measured.<ref name="Akan Tourist Assoc">Template:Cite web</ref>
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.<ref name="Hunt">Template:Cite book</ref> A local legend says that if a person can see the surface of the lake, they will have bad luck.<ref name="Akan Tourist Assoc" />
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 the Japanese name originated from the Ainu Mas-un-to or lake of the gulls.<ref>Template:Cite web</ref> This was then rendered as Template:Nihongo by the Japanese. Over time, however, the Japanese began to refer to the lake by the Japanese reading for the neighboring peak, Template:Nihongo.<ref name="Sanpei">Template:Nihongo, Template:Nihongo, page 128, (in Japanese).</ref> 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.<ref name="Hunt" /> 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.<ref>Template:Cite web</ref>
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.<ref name="Seamless">Template:Cite web</ref>
The following table lists the eruptions of the Mashū volcano and Kamuinupuri.<ref name="Smithsonian">Template:Cite gvp</ref>
| Volcano | Date of eruption | Dating technique | VEI | Tephra volume | Type |
|---|---|---|---|---|---|
| Mashū | 7400 BC ± 200 years | Corrected radiocarbon | 4 | Template:Convert | Explosive eruption |
| Mashū | 6600 BC ± 50 years | Corrected radiocarbon | 6 | Template:Convert | 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 | Template:Convert | Explosive 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.<ref name="Bisignani" /> 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.<ref name="ILEC" />
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
References
External links
- Mashu - Japan Meteorological Agency Template:In lang
- Template:Cite web - Japan Meteorological Agency
- Mashu - Geological Survey of Japan
- Mashu: Global Volcanism Program - Smithsonian Institution
- Teshikaga navi - Teshikaga Town