Glacier National Park [Montana]United States. Department of the Interior
History
Glacier National Park [Montana]
United States. Department of the Interior
Glacier National Park (Mont.)
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.
[Illustration: _Grant photo._ HORSEBACK PARTY ON BOULDER PASS]
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.
Public-domain text, read in full here on John Shaqi.
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