There are glacial erratics, so why not a stream erratic? This is a shot from two years back at a favorite location in the Quabbin Watershed-Atherton Brook inside Gate 15 in Shutesbury. I haven’t been back here this year so I am not sure if the rock is still balanced there or not. Sounds like a good hike for the weekend some time. With all the branches and chunks of ice that flow in the Spring one would imagine it received a bump or two at some point.
I hope the title didn’t cause anyone to send the children off to bed before opening this up. 🙂