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Bathurst Inlet, a southeastern extension of Coronation Gulf, penetrating the arctic shore for some 200 km. The hamlet of Bathurst Inlet is located at the mouth of the Burnside River, which drains Contwoyto Lake to the southwest.

Labrador Sea is the body of water between Greenland and the coast of Labrador. It is 3400 m deep and 1000 km wide where it joins the North Atlantic and shallows to less than 700 m where DAVIS STRAIT separates it from BAFFIN BAY.

Koksoak, Rivière, 874 km long (to head of Caniapiscau River), final leg of a river system that drains a vast area (133 000 km2) of northern Québec.

Lac la Martre, 1777 km2, elev 265 m, max length 76 km, is located in the Northwest Territories, 50 km west of Behchokò and 150 km northwest of Yellowknife, and 346 km south of the Arctic Circle. The settlement of WHATÌ is located at the southeastern corner of the lake.

Cabot Strait, the passage between southwest Newfoundland and Cape Breton Island. Named for explorer John Cabot, it is 110 km wide between Cape Ray, Nfld, and Cape North, NS.

Mount Edith Cavell, elevation 3368 m, the highest mountain in the environs of Jasper, Alberta, is situated west of the Athabasca River, 24 km south of Jasper.

The Toronto Islands, 332 ha, are an archipelago of 15 islands in Lake Ontario about 1.6 km south of downtown Toronto.

At 3,185 km (1,149 km of which lie in Canada), the Yukon River is the fifth-longest river in North America.

The Salish Sea, approximately 18 000 km2, is comprised of the inland marine waters of Juan de Fuca Strait, the Strait of Georgia and Puget Sound, as well as their connecting channels, passes and straits.

Dean River, 241 km long, world-famous steelhead- and salmon-fishing stream, rises in the Fraser Plateau of west-central BC, flows northwest and west through the COAST MOUNTAINS and empties near the head of Dean Channel.

The paucity of precipitation in deserts is due to one or a combination of causes.

Although the other limits are less well defined, the highlands may be considered to extend 100-200 km northward from the scarps and to stretch from the Gatineau River in the west (mean elevation 400 m) some 550 km to the SAGUENAY RIVER in the northeast.

Kettle Valley is a dry, forested area in the Okanagan Highland of southern BC. The name relates either to rock formations in the waterfalls at the confluence of the Kettle and COLUMBIA rivers in Washington state or to the shape of baskets woven by Salish people there.

Kane Basin is a broad expanse of water, about 3900 km2, that leads northward between the eastern shore of ELLESMERE ISLAND and the west coast of Greenland. It is relatively shallow; for the most part depths reach 180 m. Ice conditions are a severe impediment to navigation.

Kazan River, 850 km long, rises near Kasba Lake in southern Nunavut near the Saskatchewan border. Flowing north it follows an irregular course through several lakes, draining a large part of the Barren Lands.

Formed of ancient Precambrian rocks and heavily glaciated during the Quaternary (1.65 million to 10 000 years ago), the mountains support more than 70 small glaciers, the southernmost in eastern North America.

Kootenay Lake, 407 km2, elev 532 m, is situated in the mountainous southeastern interior of BC.

La Grande Rivière, 893 km long, rises in the rugged forest highlands of central Québec and drains west into James Bay.

The Kawartha Lakes are interconnected lakes in south-central Ontario.

Kicking Horse Pass is a route through the Rocky Mountains. At an elevation of 1,627 m, Kicking Horse Pass straddles the Continental Divide on the border between Alberta and British Columbia in Yoho National Park. In 1971, Kicking Horse Pass was designated a National Historic Site for its importance as a transportation corridor in Western Canada, first for Indigenous peoples, then the Canadian Pacific Railway, and finally the Trans-Canada Highway.