SPOTLIGHT: How were they formed?
The distinctive circular potholes are a direct result of glacial activity some 9,500 years ago. Specifically, it's a result of something known as swirling. When glaciers melt, they send huge amounts of water flowing at an incredible rate across the terrain. And because of the sheer force, they push whatever rocks and debris may be in the way. Now, when small rocks get caught onto larger ones, they end up spinning in circles. This sounds bizarre, but they basically swirl around in circles so fast that they drill themselves into the ground. The diagram below visualizes this, showing this unique action taking place. There are two main potholes in the park, and the bigger one is easier to access. Visible from the start of the boardwalk, it is cool to think about how rocks spinning in circles after a giant ice age would cause these kettle-looking holes. I certainly recommend reading the informative signs around the park, because they teach these prehistoric stories well.