Hudson Bay drainage basin
The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about , the basin is almost totally in Canada (spanning parts of the Prairies, central and northern Canada), with a small portion in the United States (in Montana, the Dakotas, and Minnesota). The watershed's headwaters are in part on the Continental Divide of the Americas, and the watershed's connection to the Labrador Sea is at the Hudson Strait's mouth between Resolution Island in the Qikiqtaaluk Region and Cape Chidley on the Labrador Peninsula. On the Continental Divide the basin is bounded at Triple Divide Peak to the south, and Snow Dome to the north.
Kootenay River
The Columbia Basin is noted for its spring floods, major flood years were 1876, 1894, 1948 and 1964. As recently as the mid-1960s, the upper Columbia and Kootenay rivers in British Columbia were still free-flowing and unaffected by dams and reservoirs, resulting in the 1948 Vanport Oregon flood. The uncontrolled discharge past the Canada-U.S. border created problems for electricity generation in the US, and Canada also wanted to utilize the Columbia river for the production of hydroelectric power. Negotiated in 1961 between the governments of the two countries, the Columbia River Treaty attempted to ratify these problems. Construction of the first three of the four dams authorized by the treaty—Mica, Keenleyside and Duncan—was implemented in 1964. Of the four dams, the first two are on the Columbia, the third is on the Duncan River, a tributary of the Kootenay, and the fourth Libby, on the Kootenay River proper. However, operation of the dams has led to environmental problems in both rivers because they have caused unnatural flow fluctuations, blocked fish migration, flooded fertile agricultural land, and forced over 2,000 people to relocate.