Around 31,500 years ago, as the Earth began to warm up at the tail end of the Ice Age, the expansive ice sheets (glaciers) that blanketed the region began melting and moving north. This process of melting and receding carved out valleys and paths for rivers and left behind morraines, kames, and bogs preserved in the Kettle Moraine park units and the 8-mile long lake the Potawatomi called Kishwauketoe (“Clear Water”), eventually known as Geneva Lake. These natural landmarks serve as the backdrop for the local farmers and businesses looking to shift to more sustainable practices. The following are some of the most notable to support.