| Lake Abashiri 網走湖 |
|
|---|---|
| Lake frozen over (February 2004) | |
| Location | Abashiri, Hokkaidō, Japan |
| Lake type | Dimictic |
| Primary inflows | Abashiri River and Memanbetsu River |
| Primary outflows | Abashiri River |
| Catchment area | 1,380 km2 (530 sq mi) |
| Basin countries | Japan |
| Surface area | 33 km2 (8,200 acres) |
| Average depth | 7.2 m (24 ft) |
| Max. depth | 16.1 m (53 ft) |
| Water volume | 0.2327 km3 (0.0558 cu mi) |
| Residence time | 0.43 years |
| Shore length1 | 44 km (27 mi) |
| Surface elevation | 0.4 m (1.3 ft) |
| Frozen | December to April |
| Islands | none |
| Settlements | Abashiri |
| 1 Shore length is not a well-defined measure. | |
Lake Abashiri (網走湖 Abashiri-ko) is a lake in Abashiri, Hokkaidō, Japan.[1] It is located in Abashiri Quasi-National Park. The Abashiri and Memanbetsu Rivers flow into the lake. Water exits the lake through the Abashiri River again and flows 7 kilometres (4.3 mi) to the Sea of Okhotsk.[2]
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From core samples taken from the lake bed, the lake basin appears to have first formed some 20,000 years ago during the last period of glaciation. During the last 6000 years, the Abashiri River carved out the lake bed. Artifacts from the Jōmon period have been found in the area around the Memanbetsu River. In modern times, the course of the Abashiri River has been straightened to provide for irrigation resulting in a serious siltation problem for the lake.[2]
The lake freezes over from December to April with ice up to a meter thick. The reduced inflow of water during the winter season causes saltwater to flow upstream from the Sea of Okhotsk and into the lake. This influx of saltwater has created a layer of water with 10,000 ppm of chlorine, 10 metres (33 ft) below the surface of the lake.[2]
Delta smelt, chum salmon and cherry salmon are the most important sport-fish. In 1980, approximately 650 tons of fish were caught. Ice Goby (Leucopsarion petersi) can also be found in the lake.[2]