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At the end of the last ice age, humans started to inhabit the mountain range.After Europeans, such as Sir Alexander Mackenzie, and Americans, such as the Lewis and Clark expedition, started to explore the range, minerals and furs drove the initial economic exploitation of the mountains, although the range itself never became densely populated.The eastern edge of the Rockies rises dramatically above the Interior Plains of central North America, including the Sangre de Cristo Mountains of New Mexico and Colorado, the Front Range of Colorado, the Wind River Range and Big Horn Mountains of Wyoming, the Absaroka-Beartooth ranges and Rocky Mountain Front of Montana and the Clark Range of Alberta.In Canada geographers define three main groups of ranges: the Continental Ranges, Hart Ranges and Muskwa Ranges (the latter two flank the Peace River, the only river to pierce the Rockies, and are collectively referred to as the Northern Rockies).The range's highest peak is Mount Elbert located in Colorado at 14,440 feet (4,401 m) above sea level.

See Rivers of the Rocky Mountains for a list of rivers.Jackson Hole, Wyoming, increased 260%, from 1,244 to 4,472 residents, in 40 years.The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces.The Muskwa and Hart Ranges together comprise what is known as the Northern Rockies (the Mackenzie Mountains north of the Liard River are sometimes referred to as being part of the Rocky Mountains but this is an unofficial designation).The western edge of the Rockies includes ranges such as the Wasatch near Salt Lake City and the Bitterroots along the Idaho-Montana border.

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The angle of subduction was shallow, resulting in a broad belt of mountains running down western North America.

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