The geologic forces of heat, pressure, deposition, uplift and erosion have combined with millions of years of time to create the spectacular setting for the carving of
There are two distinct stories to tell - the origin of the rocks and the creation of the current topography. The rocks are ancient, the topography is relatively recent.
Origin of the Rocks
There are two main types of rock at
The metamorphic rocks we now see began as sediments at the bottom of a shallow sea during the Precambrian period - sometime between 1.6 and 2.5 billion years ago. Dates this old are very difficult to determine precisely, mainly because they pre-date all life on the earth. What is now western South Dakota was then near the edge of a sea. Because there was no plant life to hold the forces of erosion in check, erosive forces acted much faster during the Precambrian. Vast quantities of sand and clay were washed down into the sea.
Formation of the Granite
About 1.6 billion years ago a great mass of molten rock began to rise from deep within the earth's crust. As this mass cooled (still well underground) it formed the granite which is now the core of the Black Hills. The molten rock cooled unevenly, forming both blocks of relatively fine grained rock (quick cooling) and, more commonly, blocks of coarse grained pegmatite (slow cooling). A large block of fine grained granite now forms the upper portion of Mount Rushmore, providing an excellent carving medium for Gutzon Borglum.Metamorphism
As this mass of molten rock rose upwards it came in contact with the older sandstone and shale. The intense heat and pressure melted some of the sedimentary rocks and turned the rest into metamorphic rock. The sandstone became quartzite, an extremely hard, glassy rock. The more abundant shale became mica schist. What had once been shale now acquired a property called schistosity, or the physical ability to break easily into thin slices. The mineral content was also changed by the pressure as the original quartz and clay were converted into new minerals. The most common are muscovite and biotite, but others include garnet, sillimanite, staurolite, cordierite and feldspar. The rocks were also bent and folded. The exact contact points between the granite and the metamorphic rocks can be seen in many places within the memorial as geologic unconformities. These granites and metamorphic rocks (mainly mica schists) make up all of the surface rock visible within the memorial.
Formation of the Topography
The geologic history of the region between 1.6 billion and 500 million years ago is unknown. Either no rocks formed during that time or none have survived. Several miles of rocks must have been eroded from above the granite during that time, creating marine sediments which have been found to the east of the region.
The flanks of the
About 70 million years ago the area of the
The primary erosive forces in action today are wind, rain, snow and frost wedging. The forces of wind and weather slowly eat away at the rocks of the memorial. However, the granite is extremely resistant. The rate of erosion on the granite faces has been estimated at only 1/10 inch per one thousand years.
A more significant erosional force in the
What You See Today