Kames are small, hill-like landforms created by the movement of glaciers. They are typically formed from the accumulation of sediment and debris that glaciers transport and deposit as they advance and retreat. Kames can vary in size and shape, often appearing as mounds or ridges in the landscape. These landforms are commonly found in regions that experienced glaciation, such as parts of North America and Europe. Kames are important for understanding past glacial activity and can also influence local ecosystems by providing unique habitats for various plant and animal species.