Wisconsin's moraines, up to 300' high, and related glacial features, are considered among the most impressive in North America.

Most of the large glacial features are south of the Trans-Canada corridor.

Because of such a history with ice, glacial features are readily found on the landscape, such as moraines and kames.

Then from 25,000 to 10,000 years ago the lower volume Wisconsin glaciation carved many of the glacial features seen today.

To the west drainage enters the lake through deeply cut ravines in glacial features forested with hemlock and pine.

In glaciated sections, steep canyons developed and much of the terrain have many glacial features.

In Central Park, for example, much of the visible bedrock was shaped by ice, and unmodified glacial features abound.

The Prokletije are a typical high mountain range with a pronounced steep topography and glacial features.

All are more than 13,000ft high, with dramatic glacial features that earned the region Unesco natural heritage status.

The glacial features in the Menzenschwand valley are even more striking.