A picturesque cut-off highway over aspen-covered foothills around the very base of majestic Chief Mountain, and beginning at a point 4 miles north of Babb, leads to Waterton Lakes Park in Canada.
Trails lead from the village to principal points of interest in the Canadian Park as well as up the west shore to the head of the lake at which are situated the Government ranger station and Goathaunt Camp. The head of the lake is more readily reached by the daily launch service from Waterton Village, or over trail from Many Glacier by Crossley Lake Camp, or by Granite Park and Flattop Mountain. A scenic trail leads to Rainbow Falls and up Olson Valley to Browns Pass, Bowman Lake, Hole-in-the-Wall Falls, Boulder Pass, and Kintla Lake in the northwest corner of the park. There are no hotel or camp accommodations at Bowman or Kintla Lakes.
Game is varied and abundant at Waterton Lake. Moose are sometimes seen in the swampy lakes along Upper Waterton River. Later in the season, bull elk are heard bugling their challenge through the night. Deer are seen both at Waterton Lake Village and Goathaunt Camp. Sheep and goats live on neighboring slopes. One does not have to leave the trail to see evidence of the work of the beaver. The trail down Waterton Valley has had to be relocated from time to time, as these industrious workers flooded the right-of-way. A colony lives at the mouth of the creek opposite Goathaunt Camp. Otters have been seen in the lakes in the evening. Marten have bobbed up irregularly at the ranger station.
Bird life is abundant in this district, because of the variety of cover. Waterfowl are frequently seen on the lake. A pair of ospreys nest near the mouth of Olson Creek. Pine grosbeaks, warblers, vireos, kinglets, and smaller birds abound in the hawthorne and cottonwood trees, and in the alder thickets.
FLATTOP MOUNTAIN AND GRANITE PARK
Glacier Park has within its boundary two parallel mountain ranges. The eastern, or front range, extends from the Canadian boundary almost without a break to New Mexico. The western, or Livingston Range, rises at the head of Lake McDonald, becomes the front range beyond the international line, and runs northwestward to Alaska. Between these two ranges in the center of the park is a broad swell which carries the Continental Divide from one to the other. This is Flattop Mountain, whose groves of trees are open and parklike, wholly unlike the dense forests of the lowlands with which every park visitor is well acquainted.
A trail leads south from Waterton over Flattop to the tent camp called "Fifty Mountain" and to Granite Park, where a comfortable high-mountain chalet is located. Here is exposed a great mass of lava, which once welled up from the interior of the earth and spread over the region which was then the bottom of a sea. The chalets command a fine view of the majestic grouping of mountains around Logan Pass, of the noble summits of the Livingston Range, and of systems far to the south and west of the park. Extending in the near foreground are gentle slopes covered with sparse clumps of stunted vegetation. In early July open spaces are gold-carpeted with glacier lillies and bizarrely streaked with lingering snow patches. Beyond are the deep, heavy forests of Upper McDonald Valley.