While Arches National Park in northeastern Utah is best known for its hundreds of red rock arches, many rock formations are almost equally as famous. Balanced Rock is one of the more well known, as it is easily seen from the main road in the park.
The uppermost part of Balanced Rock, a strong type of rock called Slick Rock sandstone, rests on a less stable rock known as Dewey Bridge mudstone. Since the mudstone erodes faster than the Slick Rock, top-heavy formations occur with some frequency. Eventually the weaker pedestals will wear away and Balanced Rock will collapse.
At dusk, the red hues of the rock are intensified, and it is quite impossible to drive past the rocks and not stop for a photograph. I would imagine anyone who has ever visited Arches has a photograph similar to this one.