East of the river, moraines and small kettle lakes are interspersed throughout the plain.

The kettle lakes are predominantly confined to the northern fringes of the town.

When kettles fill with water, they are known as kettle lakes.

It is the largest kettle lake in North America.

Lake Matheson formed as a kettle lake within one of these.

It is a kettle lake and has no tributaries or outlets.

Whitchurch-Stouffville is also home to a number of kettle lakes which are ideal for outdoor water recreation.

The kettle lake was made in the last ice age by the glacier that covered 2/3 of Ohio.

In between them lie the tunnel valley lakes and kettle lakes.

Other notable features of the park include a kettle lake, and talus slope.