Okanagan Lake: Difference between revisions

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m Changed the quantity of islands in Okanagan Lake from two to four
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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 River|Columbia]].
 
The lake's maximum depth is {{convert|232|m}} near [[Grant Island (Okanagan Lake)|Grant Island]] (Nahun Weenox). There isare onethree other islandislands: one known as [[Rattlesnake Island (Okanagan Lake)|Rattlesnake Island]], much farther south by Squally Point. The other two are near Grant Island. They are unnamed and are located just north of the north-point of Whisky Cove at Carrs Landing.Some areas of the lake have up to {{convert|750|m}} of glacial and post-glacial sediment fill which were deposited during the [[Pleistocene Epoch]].<ref name="eyles90" />
 
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.