The Geologic Story of Glacier National ParkDyson, James L. (James Lindsay)
Science
The Geologic Story of Glacier National Park
Dyson, James L. (James Lindsay)
Geology -- Montana -- Glacier National Park; Glacier National Park (Mont.)
This is the oldest of the several formations and thus occupies a
stratigraphic position at the base of the entire series. It is composed
mainly of sandy dolomites (magnesian limestones) and limestones which
weather to a light buff color. It outcrops all along the base of the
eastern front of the Lewis Range and comprises the entire block of Chief
Mountain. Because of its comparatively great resistance to weathering
and erosion it usually forms a conspicuous ridge or terrace wherever it
crosses a valley. In the Swiftcurrent Valley it forms the dam which
holds in Swiftcurrent Lake and creates Swiftcurrent Falls. In Two
Medicine Valley the highway crosses a similar terrace which gives rise
also to Trick Falls. In the St. Mary Valley it creates the Narrows and
forms the imposing wall in lee of which East Glacier Campground is
located. The rock of this formation can best be examined on the ridge
immediately east of Many Glacier Hotel (between hotel and parking lot)
and above Swiftcurrent Falls. Its average thickness is about 2,300 feet.
APPEKUNNY FORMATION.
Lying on top of the Altyn are 3,000 or more feet of prevailing greenish
shales and argillites[2] comprising the Appekunny formation. Slabs of
these rocks, because of their great hardness, have been used as
flagstones in the walks at the Many Glacier Ranger Station and adjacent
Park Service residential area. Mud cracks and ripple marks are common.
The formation is prominent on the side of Singleshot Mountain near the
St. Mary entrance to the park, and everywhere immediately overlying the
lighter-hued Altyn along the east edge of the Lewis Range where,
especially when seen from a distance, it appears to have a purplish
color. It also outcrops along the western base of the Livingstone Range
(Figure 3D), but such exposures are as a rule obscured by a cover of
dense forest. Accessible outcrops can readily be examined along
Going-to-the-Sun Highway for several miles east of Sun Point and near
McDonald Falls, and also along the lower part of the Grinnell Glacier
trail.
GRINNELL FORMATION.
Public-domain text, read in full here on John Shaqi.
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