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  1. Locations

Rocky Mountains

Natural Feature

The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 mi (4,800 km)[1] in straight-line distance from the northernmost part of British Columbia, in western Canada, to New Mexico in the Southwestern United States. The northern terminus is located in the Liard River area east of the The Pacific Coast Ranges, while the southernmost point is near the Albuquerque area adjacent the The Albuquerque Basin (Middle Rio Grande Basin) and north of the The Sandia–Manzano Mountains. Located within the North American Cordillera, the Rockies are distinct from the tectonically younger The Cascade Range and The Sierra Nevada, which all lie farther to the west.

The Rocky Mountains formed 80 million to 55 million years ago during the Laramide orogeny, in which a number of plates began sliding underneath the North American plate. The angle of subduction was shallow, resulting in a broad belt of mountains running down western North America. Since then, further tectonic activity and erosion by glaciers have sculpted the Rockies into dramatic peaks and valleys. At the end of the last ice age, humans began inhabiting the mountain range. After explorations of the range by Europeans, such as Sir Alexander Mackenzie, and Anglo-Americans, such as the Lewis and Clark expedition, natural resources such as mineral and fur drove the initial economic exploitation of the mountains, although the range itself never experienced a dense population.

Of the 100 highest peaks in the Rocky Mountains, 78 (including the 30 highest) are located in Colorado, ten in Wyoming, six in New Mexico, three in Montana, and one in Utah. Public parks and forest lands protect much of the mountain range, and they are popular tourist destinations, especially for hiking, camping, mountaineering, fishing, hunting, mountain biking, skiing, and snowboarding.