The principal highway through the Cub Hills is Highway 106, also known as the Hanson Lake Road, which begins at Smeaton and travels north into the hills then east to Flin Flon and the border with Manitoba. Other highways through the hills include 120, 912, 913, and 920.[5]
Geography
The glaciers retreated from the area about 10,000 years ago. And in their wake, they created many of the landforms in and around the Cub Hills, such as the valleys, lakes, and lowlands. Throughout the plateau, evidence left behind by the glaciers includes deposits of eskers and push moraines and tunnel valleys, which were created by subglacial erosion by meltwater. Many of the lakes, known as potholes, were created by depressions caused by dead ice when the glaciers were receding.
Boreal forest, muskeg, rolling hills, and small lakes and rivers are prominent features of the landscape today.
Lakes and rivers
The Cub Hills are entirely within the Hudson Bay drainage basin. Most of the hills are part of the Saskatchewan River watershed, including the northern, eastern, and southern slopes. The western slope of the hills flows north through the tributaries of the Nipekamew River, which flows into Lac la Ronge then the Churchill River via the Rapid River. The waters of the northern slope work their way north into various tributaries of the Sturgeon-Weir River, which meets up with the Saskatchewan River near the Manitoba border after going through Namew Lake, Whitey Narrows, and then Cumberland Lake of the Saskatchewan River Delta. The eastern slope of the hills is drained by the Mossy River and its tributaries into the Saskatchewan River Delta. Several rivers flow south out of the hills and into the east-flowing Torch River — a tributary of the Saskatchewan River.
Narrow Hills Provincial Park,[8] originally established in 1934 as Nipawin Provincial Forest, covers much of the southern portion of the Cub Hills. The park has over 25 lakes, multiple campgrounds, lodges, and a wide network of trails for hiking, snowmobiling, and ATVing.[9]