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Williston Lake, 1761 km2, is the largest freshwater body in BC. Created in 1968 as the reservoir of the W.A.C.

Wollaston Lake, 2681 km2, elev 398 m, lies in the wooded Shield country of NE Saskatchewan.

The lake lies in a lowland basin that was scoured out of the limestone and shale bedrock by continental glaciers during the ice ages. When the glaciers finally melted, about 12 000 years ago, a large lake, Glacial Lake AGASSIZ, filled the entire basin.

Winisk River, 475 km long, rises in Wunnummin Lake in the Kenora District of northern Ontario.

Winnipegosis, Lake, 5370 km2, 195 km long, elev 254 m, maximum depth 12 m, Canada's eleventh-largest lake, is located in west-central Manitoba.

Origins Lava tube caves, an important minor class, are formed by channelled outflow of molten lava in congealing flows. Sea caves most commonly result from erosion by waves.

The Hillsborough River begins near the white sand beaches of the north shore and winds 45 km through rich farm country to its mouth (Charlottetown Harbour) on the south shore of Prince Edward Island. At its mouth, the North and West rivers come together to meet the Hillsborough.

The Soper River winds southwards 108 km through the tundra-covered hills of southern Baffin Island before emptying into Soper Lake, a brackish water body, and then directly into Hudson Strait near the community of Kimmirut, Nunavut.

Mount Steele, elevation 5067 m, is located among Canada's highest mountains in the St Elias Range of Yukon.

Lake Abitibi, 932 km2, elev 265 m, straddles the Québec-Ontario border about 280 km south of James Bay.

Avalon Peninsula, 9220 km2, is a spreading peninsula thrust out into the rich fishing grounds of the north Atlantic, forming the southeast corner of insular Newfoundland.

The Parry Islands are a group of high arctic islands comprising Melville, Bathurst and Cornwallis islands, as well as a number of smaller ones. Melville is the largest of the 3 main islands and is also the highest, exceeding 1000 m in places.

Port Refuge is a small bay on the south coast of Grinnell Peninsula, Devon I, in the high Arctic.

Nass River is 380 km long, rises in the northern interior of BC and flows generally southwest, draining approximately 20 700 km2, to reach the Pacific at Portland Inlet. Its major tributaries are the Bell-Irving, Meziadin and Cranberry rivers.

Mount Vancouver, elevation 4785 m, situated in the Yukon Territory's St Elias Mountains, rises southeast of Mount Logan between 2 immense glacier systems, Hubbard and Seward.

Tucked into the westernmost corner of Prince Edward Island, Cedar Dunes Provincial Park (established 1962, 37 ha) has been developed around an historic lighthouse. Known as West Point, the site is the result of centuries of accretion of sand from a north to south coastal current.

Sverdrup Islands, located in the High Arctic, comprise a large island, Axel Heiberg, and two smaller ones, Ellef Ringnes and Amund Ringnes. Their geological history began as an area of subsidence and sedimentation on a landmass margin.

Red Lake, Ontario, incorporated as a municipality in 1998, population 4,107 (2016 census), 4,366 (2011 census). The municipality of Red Lake is located in northwestern Ontario on the shore of Red Lake, 555 km northwest of Thunder Bay. The municipality is the result of the amalgamation of the former townships of Red Lake (incorporated in 1960) and Golden (established in 1985), and the unorganized territory governed by the Madsen local services board. Red Lake consists of six communities (Madsen, Red Lake, Balmertown, Cochenour, McKenzie Island and Starratt-Olsen) that sprang up around the area's gold mines.

In contrast to the soft, white limestone cliffs of the west shore, the east shore is cut into the hard edge of the Canadian Shield, fractured into myriad bays, inlets and sounds, with thousands of islands strewn along the coasts.