Photo credit: B. Bednarek, Parnell Segment, view from Parnell Tower

Did you know, world famous glacial landscape features are within an easy drive from your front door?

This might not seem like such a big deal until you consider that walking across the high ridge of an esker, or peering down into a kettle lake is a bit like time travel, giving you a peek into how the landscape of Wisconsin was formed.

Conveniently, the almost 30,000 acres of the Northern Kettle Moraine State Forest contains some of the most stellar glacial remnants of the last Ice Age. In fact, this region was formed as two tongue-shaped ice sheets collided, creating a valley of ice some 10,000 years ago. As these huge sheets of ice melted, the meltwater cascaded into crevasses carrying sand, gravel, and boulders, depositing them along the way. This is what shaped the rolling ridges and deep kettles – large crater-like depressions – that make up the topography of this beautiful forest. Continue reading →