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Weinberge im Okanangan Valley, BC, Canada - PIP
PIP - Die Winzer dort haben noch recht bescheidene Anwesen
Okanagan Lake ist ein langer, schmaler Binnensee in der kanadischen Provinz British Columbia. Der rund 135 km lange und 4-5 km breite See mit einer Oberfläche von 351 km² schlängelt sich im südlichen Teil von British Columbia durch das Okanagan-Becken und geht rund 55 km vor der Grenze zum US-Bundesstaat Washington in den gleichnamigen Fluss über.
Die größte Stadt am Ufer des Sees ist mit 117.312 Einwohnern Kelowna, die sich Anfang des 20. Jahrhunderts entwickelte, als zahlreiche Europäer das Tal besiedelten. Die Bewohner entlang des Sees, darunter viele deutschstämmige Kanadier, leben insbesondere vom Fremdenverkehr, sowie von der Land- und Forstwirtschaft. Insbesondere in Kelowna entwickelte sich zudem ein ertragreiches Dienstleistungsgewerbe. Die Gegend ist innerhalb von Kanada insbesondere für den Anbau von Obst und Wein bekannt.
Der Legende nach lebt im Okanagansee das Seeungeheuer Ogopogo.
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.[7] 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 Pleistocene Epoch.
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. Q:Wikipedia
Okanagan Lake ist ein langer, schmaler Binnensee in der kanadischen Provinz British Columbia. Der rund 135 km lange und 4-5 km breite See mit einer Oberfläche von 351 km² schlängelt sich im südlichen Teil von British Columbia durch das Okanagan-Becken und geht rund 55 km vor der Grenze zum US-Bundesstaat Washington in den gleichnamigen Fluss über.
Die größte Stadt am Ufer des Sees ist mit 117.312 Einwohnern Kelowna, die sich Anfang des 20. Jahrhunderts entwickelte, als zahlreiche Europäer das Tal besiedelten. Die Bewohner entlang des Sees, darunter viele deutschstämmige Kanadier, leben insbesondere vom Fremdenverkehr, sowie von der Land- und Forstwirtschaft. Insbesondere in Kelowna entwickelte sich zudem ein ertragreiches Dienstleistungsgewerbe. Die Gegend ist innerhalb von Kanada insbesondere für den Anbau von Obst und Wein bekannt.
Der Legende nach lebt im Okanagansee das Seeungeheuer Ogopogo.
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.[7] 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 Pleistocene Epoch.
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. Q:Wikipedia
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