The spacious path provides a gentle, unobstructed hike along the busiest trail system in the Rocky Mountain park system. An avalanche slope is exposed at km 1, a reminder of how dynamic these otherwise stable giants can be. This expanse of openness is the first of two rises before arriving at Kinney Lake Campground, but with only 70 m of elevation gain over 500 m it is quite effortless. Before the track fades back into the forest at the top of this knoll, there is a dazzling view of Mt. Robson, straight up the way.
The wide trail, wide enough to walk side by side, meanders through a magnificent old-growth forest of Douglas fir, cedar, hemlock and spruce. The sight of these huge trees is breathtaking. They are truly glorious. This is unlike any forest in the Rocky Mountain park system. Even the damp odours from the ferns, mosses, lichens and fungi are exceptional. These natural surroundings remain unchanged until you reach the bridge over the Kinney Lake outlet at the 4.5-km mark. This tranquil setting is a popular spot to stop and rest, as the serene, fast, yet smoothly flowing stream quickly becomes intoxicating. Or maybe it is just popular because there’s an outhouse in the forest on the other side of the bridge.
Back into the lush forest, the path narrows as it sidesteps the lake. Another kilometre along, the second rise on this route begins to climb through a series of switchbacks. The trail to the Kinney Lake viewpoint intersects to the left partway through this modest elevation gain. It is worth the momentary detour along a well-constructed boardwalk to observe the lake from this precipice. The hike continues to ascend briefly, levels out, then descends to the lakeside once again.
The approach to the campground spans an outwash pan of sand and gravel. This entanglement of streams can present a minor inconvenience during high glacial runoff and you should utilize the wooden platforms provided for this crossing. Tent pads are available along the shoreline entering the campground that can be used to offset the effects of a hot summer day. More-protected tent pads are at hand in the forest surrounding the main campground. The common campsite area opens up with an impressive shelter at its heart that functions as a cooking area and meeting place. Splendid lakeside viewing is offered here along this treeless shoreline.
Kinney Lake is an archetypal glacier-fed lake, owing its aquamarine hue to its purity, enabling short-wavelength light to be reflected off tiny mineral particles ground by glaciers. The valley that this dazzling lake resides in was gouged out by retreating ice during the late Pleistocene period of glaciation, 30,000 to 21,000 years ago. As the ice melted, the resulting water filled gouged-out low spots to form the lake. Today, the lake’s source resides in the Robson glacial system: the combined Berg, Mist and Robson glaciers on the north rampart of Mount Robson. This system also nourishes Berg Lake and the Robson River. Directly across Kinney Lake, Cinnamon Peak and Whitehorn Mountain to the north (right) rise to confine the southwest shore of the lake. Drainage from snowpack in these mountains produces waterfalls that cascade hundreds of metres down the rock walls and into the lake.
Day trips from the campground depend on your stamina. The only direction is to go farther up the trail. This and much more about Berg Lake are discussed in the Whitehorn Campground