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About 350 million years ago, the Antler orogeny

(see link below) began to deform the Paleozoic rocks of Nevada's Great Basin and western Utah to lay down the basis of what would become The Rockies. For 270 million years, the Antler volcanic island arc terrane collided with the western coastal area of the North American plate, near what is today's border area of Nevada and Utah.
The current Rockies came up between 80 and 55 million years ago during what is called the Laramide orogeny

(see other link below), with the growth of the southern part of the Rockies believed to have been caused by the subduction of the Farallon plate taking a shallowly-angled dive beneath the North American plate.

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