Glacier N.P.; Montana

     The first week of July in 2016, Becky (my wife) and I took a week long road-trip to Montana to visit Glacier National Park.

Area map of Glacier National Park, Montana 2016

     Majestic peaks, glacial trough, lakes, and the Continental Divide make up Glacier National Park. The mountains in the Glacier National Park region are described as “mountains without roots” because they consist of ancient Precambrian rocks resting on top of much younger sedimentary beds.  The reason for this is that a huge, low-angled thrust fault, known as the Lewis Overthrust fault, transported the sequence of Precambrian rocks eastward for many miles over the younger rocks.

This simplified geological cross section of Glacier National Park image is found at

     The layered rocks in Glacier National Park are part of a thick series of sedimentary rocks called “the Belt rocks” or more formally, the Belt Super-group.  What makes these rocks so unusual is that they are relatively undeformed and only lightly metamorphosed despite the fact that they were deposited fairly late in Precambrian time, (1600 – 800 million years ago).  

Stratigraphy description of the “Belt Rocks” found within the Glacier National Park.

     Pictured below, we visited Lake McDonald, the largest lake in the Park.

Looking north-east, Becky is standing on the shore of Lake McDonald in the Glacier N.P. 

     Surrounded on three sides by towering Rocky Mountains that rise 2,000 meters into the sky, the view is sensational, with white alpine glaciers hugging the jagged upper slopes of the mountains and lush green forests covering the lower slopes.

Next to the “Going-to-the-Sun-Road” heading towards Logan’s Pass, (Avalanche Creek). This is near the location that we had a close encounter of a Grizzly Bear.

     While Becky and I were in the Rocky Mountain Park we saw Rocky Mountain Sheep, Mountain Goats, Bald Eagles, and a Grizzly Bear.

Mountain Goats found near the road in Glacier National Park

     Below, I’m standing in front of the Lewis Mountain Range to the east, which acts as a rain block to the clouds whose moisture supports a rich, dense forest of western red cedar and hemlock trees.

Looking east toward the Lewis Mountain Range in the Glacier National Park, 2016
Becky pointing at one of the majestic peaks found in the Glacier National Park

     The glaciation that produced the spectacular, ice-sculptured landforms in Glacier N.P. was at its maximum extent during the Pleistocene Epoch.  However, the small cirque and cliff glaciers now existing in the park developed only a few thousand years ago during the “Little Ice Age”.  The park’s active glaciers are found between elevations of 2000 and 3000 m.  The perennial snowfields lie in protected areas, usually on slopes that face north or east. 

At Logan’s Pass next to the “Going-to-the-Sun-Road” is abundant in snow-fields and glaciers.

     Later, we visited St. Mary Lake, pictured on the upper right. St. Mary Lake is a beautiful, glacial blue lake in one of the most perfect settings imaginable.

Looking south-west across St. Mary Lake on the eastern side of Glacier National Park 2016

     Triple divide Peak, south of St. Mary Lake, is unique because water drains in three directions instead of two: namely, west toward the Pacific, northeast toward Hudson Bay, and southeast toward the Gulf of Mexico.

Looking across St. Mary Lake at Triple Divide Peak in the Glacier National Park
Image taken from a sign at St. Mary Lake

     On three sides it is surrounded by the steep Rocky Mountains, and on its eastern shore, it gives way to a rolling prairie and forested hills.

A gorge found on the eastern side of Rocky Mountain National Park, 2016.
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