Pikes Peak Granite - Erosion

Erosion

Over the next billion years, the now cooled granite was gradually exposed through erosion of overlying rocks. About 60 million years ago, parts of the Western U.S. were subjected to a series of uplifts, known as the Laramide orogeny, that eventually formed the modern Rocky Mountains and raised Pikes Peak to its current height. Pikes Peak, like other portions of Colorado Rockies is still being uplifted today as a part of larger tectonic processes effecting the Western United States.

Today, the Pikes Peak Batholith and Granite is exposed over a large part of the central Front Range of Colorado. It is found as far north as the southern slopes of Mount Evans west of Denver, west to South Park, and as far south as CaƱon City. The batholith is about 80 miles (130 km) long in the north-south direction and about 25 miles (40 km) wide east to west. Even more of it remains hidden underground. Geologists have found the granite at the bottom of deep wells on the plains and magnetic sensors have detected it as much as 80 miles (130 km) to the east.

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