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Pikes Peak granite is a widespread geologic formation found in the Front Range of Colorado, including on its namesake, Pikes Peak. Pikes Peak granite comprises a much larger deposit known as the Pikes Peak batholith.

A picture of Pikes Peak granite in Pike National Forest taken from the trail to the Devil's Head Lookout


About 1.08 billion years ago, a large pool of magma formed under what is now central Colorado. Some of this magma worked its way to the surface and formed volcanos similar to what we might see today in Washington and Oregon.

After the volcanic activity died away, a large mass of molten magma was left underground. Because the magma was buried about 2 miles (5 km) underground, it took thousands of years for it to cool and this created the granite that we now see on the slopes of Pikes Peak and other areas of the Front Range.


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 is actually growing to this day, but erosion has kept up with it and thus caused it to have a consistent height.

Today, the Pikes Peak batholith covers 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 Cañon 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 it at the bottom of deep wells on the plains many miles east of the Front Range.


The granite ranges in color from light pink to almost red. The pink color is due to large amounts of microcline feldspar and various iron minerals that permeate the rock. The long cooling time and the chemical composition of the original magma allowed large crystals to precipitate out of the magma. As a result, in many places the granite is very coarse grained, made up almost entirely of large crystals of feldspar, typically about a centimeter across. This makes the granite easily weathered and very crumbly. Almost every hill and slope in the Pikes Peak region is covered with thick blankets of loose gravel (scree) made up of marble-sized grains of feldspar.

In some places, the cooling process lasted long enough to form pegmatites that contain large, pure crystals of various minerals. As a result, the Pikes Peak granite is famous for its spectacular mineral specimens.

Smoky quartz crystals and topaz are found in many places in the Pikes Peak granite. Probably the most famous mineral from the area is amazonite, a bluish form of microcline feldspar that is relatively rare in other parts of the world. Many museum collections have stunning specimens of deep blue amazonite crystals studded with jet-black smoky quartz crystals.



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