The presidential faces on Mount Rushmore are dissolving, but at a geological pace so slow that Lincoln's nose will remain for another 7 million years.
A Monument of Ancient Stone
The four presidential faces are carved into a formation known as the Harney Peak Granite. This rock is part of the ancient core of the Black Hills, formed from a mass of molten rock that rose from deep within the earth's crust about 1.6 billion years ago. The magma cooled slowly, miles beneath the surface, creating fine-grained granite composed of minerals like quartz, feldspar, muscovite, and biotite. This specific granite was chosen for the sculpture because it is massive and more resistant to erosion than the surrounding metamorphic schist rock.
The mountain itself, which stands at an elevation of 5,725 feet (1,745 meters), only became exposed after tens of millions of years of geologic uplift and subsequent erosion stripped away the softer overlying layers of rock. The durability of the granite is why the mountain is in its present form. While the surrounding, less resistant mica schist eroded into gullies and canyons, the hard granite remained, creating the prominent peak that sculptor Gutzon Borglum selected for his work.
The Geological Clock and Human Intervention
The natural erosion rate for the Harney Peak Granite is exceptionally slow, estimated at just one inch every 10,000 years. At this rate, the general shapes of the 60-foot-tall heads could remain recognizable for up to 7 million years. The primary forces of erosion at work are wind, precipitation, and, most significantly, a process called frost wedging. Frost wedging occurs when water seeps into natural cracks and fissures in the granite. As temperatures drop below freezing, the water expands by about 9 percent, exerting immense pressure that gradually widens the cracks.
To combat this, the National Park Service employs a dedicated preservation team. This team's work continues a tradition started by Borglum, who initially sealed cracks with a mixture of white lead, linseed oil, and granite dust. This original sealant proved ineffective over time as it dried out. Today, preservationists rappel down the faces to remove the old sealant and apply modern silicone-based caulking. This material is flexible enough to withstand the extreme temperature shifts on the mountain. After the silicone is applied, it is camouflaged with a dusting of granite powder collected from the site. A sophisticated electronic monitoring system, installed in 1998, uses instruments placed across major fractures to detect movement as slight as 0.0001 inches, ensuring the sculpture's long-term stability.
💡Fun Facts
Gutzon Borglum secretly began blasting a "Hall of Records" into the canyon wall behind the faces in 1938, intending it to be a vault for important U.S. documents.
The light-colored streaks visible on Washington's and Lincoln's foreheads are pegmatite dikes, which are weaker zones in the granite that formed when cracks in the cooling magma were filled by a second wave of molten rock.
The preservation team uses a specialized high-line transport system to move equipment and supplies from the base of the monument to the top of the carving.
In 2010, the entire sculpture was documented with 3D digital laser scanning to create a precise record that could be used for future preservation or even recreation.
The grounds are open year-round, except for December 25th. The Lincoln Borglum Visitor Center is generally open from 8:00 AM to 5:00 PM in the winter, with extended evening hours in the spring, summer, and fall.
Admission
There is no entrance fee for the memorial itself, but a fee is required for parking.
Accessibility
The main viewing areas and visitor center are accessible. The Presidential Trail offers the closest views of the sculpture.