The easy way to determine the age of a fir tree is to count the swirls. Each year a fir tree will send a few branches from the crown. Since they are evenly spaced around the main stem, each one is called a swirl.

A close examination shows how the forces of rain, wind, freezing, and biology are slowly eroding it. The tiny grains that get dislodged from the bolder and washed into the soil contribute minerals to the soil. This bolder was significantly larger. Based on the climate and other factors, a good estimate is that erosion will remove about 1 inch and about 8 gallons of material every 500 years. Projecting that rate over 12,000 years that this bolder has been sitting here, two feet of its surface has disappeared, while about 190 gallons of material have dissolved into the soil. In about 20,000 years from now, at this rate, it will be completely gone.

All the glacial erratics here have also experienced that magnitude of shrinkage. Since the eroding forces strike them evenly across their surfaces, it also tends to sculpt the boulders into the smooth spherical shapes you see.

As you study the boulder, you may draw other conclusions. We welcome your opinions and observations. You can contribute them below.