Steamboats of Lake Okanagan
| Okanagan Lake | |
|---|---|
 |
|
| Location | British Columbia |
| Coordinates | 49°54′40″N 119°30′45″W / 49.91111°N 119.51250°WCoordinates: 49°54′40″N 119°30′45″W / 49.91111°N 119.51250°W |
| Lake type | Fjord Lake,Monomictic, Oligotrophic |
| Primary inflows | Mission Creek, Vernon Creek, Trout Creek, Penticton Creek, Equesis Creek, Kelowna Creek, Peachland Creek and Powers Creek |
| Primary outflows | Okanagan River |
| Catchment area | 6,200 km2 (2,400 sq mi) |
| Basin countries | Canada |
| Max. length | 135 kilometres (84 mi) |
| Max. width | 5 kilometres (3.1 mi) |
| Surface area | 351 square kilometres (136 sq mi) |
| Average depth | 76 m (249 ft) |
| Max. depth | 232 m (761 ft) |
| Water volume | 24.6 cubic kilometres (5.9 cu mi) |
| Residence time | 52.8 years |
| Shore length1 | 270 kilometres (170 mi) |
| Surface elevation | 342 m (1,122 ft) |
| Frozen | 1906/07 & 1949/50 |
| Islands | Rattlesnake Island, Grant Island |
| Settlements | Vernon, Lake Country, Kelowna, West Kelowna, Peachland, Summerland, Penticton |
| References | |
| 1 Shore length is not a well-defined measure. | |
Okanagan Lake is a large, deep lake in the Okanagan Valley of British Columbia, Canada. The lake is 135 km long, between 4 and 5 km wide, and has a surface area of 348 km².
Okanagan Lake is called a fjord lake as it has been carved out by repeated glaciations. Although the lake contains numerous lacustrine terraces, it is not uncommon for the lake to be 100m deep only 10m offshore. Major inflows include Mission, Vernon, Trout, Penticton, Equesis, Kelowna, Peachland and Powers Creeks. The lake is drained by the Okanagan River, which exits the lake's south end via a canal through the city of Penticton to Skaha Lake, whence the river continues southwards into the rest of the South Okanagan and through Okanogan County, Washington to its confluence with the Columbia.
The lake's maximum depth is 232 metres near Grant Island (Nahun Weenox). There is one other island known as Rattlesnake Island, much farther south by Squally Point. Some areas of the lake have up to 750 metres of glacial and post-glacial sediment fill which were deposited during the .
Notable features of the Okanagan Valley include terraces which were formed due to the periodic lowering of the lake's predecessor, glacial Lake Penticton. These terraces are now used extensively for agriculture such as fruit cultivation.
Cities bordering the lake include Vernon in the north, Penticton in the south, and Kelowna, as well as the municipalities of Lake Country (north of Kelowna), West Kelowna (west of Kelowna), Peachland (south of West Kelowna), and Summerland (north-west of Penticton). Unincorporated communities include Naramata (north-east of Penticton).
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Wikipedia