Tazawa Lake
| Lake Tazawa | |
|---|---|
 Lake Tazawa
|
|
| Location | Semboku, Akita Prefecture |
| Coordinates | 39°43′30″N 140°39′41″E / 39.72500°N 140.66139°ECoordinates: 39°43′30″N 140°39′41″E / 39.72500°N 140.66139°E |
| Lake type | crater lake (?) |
| Primary inflows | no natural inflow |
| Primary outflows | no natural outflow |
| Basin countries | Japan |
| Surface area | 25.9 km2 (10.0 sq mi) |
| Average depth | 280.0 m (918.6 ft) |
| Max. depth | 423.4 m (1,389 ft) |
| Water volume | 7.2 km3 (5.8×106 acre⋅ft) |
| Shore length1 | 20 kilometres (12 mi) |
| Surface elevation | 290 m (950 ft) |
| 1 Shore length is not a well-defined measure. | |
Lake Tazawa (田沢湖 Tazawa-ko) is a caldera lake in the city of Semboku, Akita Prefecture, northern Japan. It is the deepest lake in Japan at 423 metres (1,388 ft). The area is a popular vacation area and several hot spring resorts can be found in the hills above the lake. Akita Prefecture's largest ski area, Tazawa Ski Area, overlooks the lake.
Lake Tazawa has a surface elevation of 249 meters, and its deepest point is 174.4 meters below sea level. Due to this depth, there is no possibility that the lake is frozen in the dead of winter. At 425 metres (1,394 ft), it is slightly deeper than Lake Shikotsu in Hokkaidō (423.4 meters), and is the 17th deepest lake in the world. Lake Tazawa has no natural inflow or outflow, and in 1931, had a measured transparency of 31 meters, comparable with Lake Mashu, but with abundant aquatic organisms. However, due to the construction of hydroelectric power plant facilities and agricultural runoff, coupled with an influx of highly acid water from Tamagawa Hot Spring, transparency has been reduced to less than 4 meters, and by the late 1940s the lake had become so acidic (pH 4.3) that it could no longer support irrigated agriculture. Starting in 1972, the Japanese government has been attempting to rectify the acidity problem through introduction of lime, with a new facility completed in 1991. However, in the year 2000, the lake still had an acidity of 5.14 at the 200 meter depth, and 4.91 at the 400 meter depth, indicating that full recovery has not yet been achieved.
Due to its extreme depth, and almost circular profile, Lake Tazawa was considered to be either a caldera lake caused by volcanic activity or a crater lake caused by a meteorite impact. The depth of the lake was first measured as 397 meters, using a hemp rope, by Japanese geologist Tanaka Akamaro in 1909. The Akita Prefectural Fisheries Experiment Station survey indicated a depth of 413 meters in 1926 using a wire rope. During a three-year survey from 1937-1940, geologist Yoshimura Nobuyoshi surveyed the lake bottom, finding the deepest point to be 425 metres (1,394 ft). The survey also found two small volcanic cones and sedimentation deposits to the depth of around one kilometer on the north-west side of the lake bottom. These findings lend credence to the theory that the lake is indeed of volcanic origin, from an explosive eruption of 1.4 million years ago.
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Wikipedia