Special Characteristics: Unsurpassed Romantic Scenery; 250 Lakes of Particular Beauty
THE Glacier National Park is so named because in the hollow of its rugged mountain tops lie more than 60 small glaciers, the remainders of ancient monsters which once covered all but the highest mountain peaks. It is in northwestern Montana right up against the Canadian boundary line, from which, on the map, it appears to hang down like a boy's pocket full of the sort of things boys usually carry there. It is a richly colored land of gigantic cirques, ruggedly modeled mountains, enormous twisting glacier-scooped valleys, precipices thousands of feet high, innumerable rushing streams, and hundreds of lakes of unusual romantic beauty. Though all the other national parks have these general features in addition to others which differentiate each from the other, the Glacier National Park possesses them in unusual abundance and especially happy combination. In fact, the almost sensational massing of these scenic features is one of the elements of its marked individuality.
Its geological history is identical with that of the Canadian Rockies, but the region lies in a much older rock formation. There is no other scenic area in the world to compare it with except the far less colorful, much snowier, and much less accessible Canadian Rockies. In richness of beauty it stands alone.
A ROMANCE OF GEOLOGY
How Nature made this remarkable area far back in the dim ages long before man is a stirring story.
In an age of the earth's making which some geologists estimate at 80,000,000 years ago, before the continent of North America had emerged in its present outlines from the sea, the shales which now loom so loftily in Glacier National Park were deposited as sediments in the waters. Over these muds thick beds of ooze solidified into limestones, and over the limestones more sediments deposited and turned to shales. It is these very strata, now hardened into rocks, that streak so picturesquely the sides of Glacier precipices thousands of feet above us. The story of their elevation from deep-sea bottoms to these giddy heights is a romantic chapter in the making of America.
The earth has assumed its present proportions through the settling of its masses, and this settling caused great internal pressures.
Often the earth's skin has broken as the skin of the squeezed orange breaks; and that is what must have happened where Glacier National Park now lies. The bottom of the sea, under the enormous pressure against its sides and from below, gradually rose and became dry land.
Then the land at this point, probably because it was pushed hard by the contracting land masses on both sides of it, rose in long irregular wavelike masses, forming mountains. Then, when the rock could no longer stand the awful strain, it cracked, and one edge was thrust upward and over the other edge and settled into its present position.
The edge that was thrust over the other was thousands of feet thick. It crumbled into peaks, precipices, and gorges.
Upon these mountains and precipices the snows and the rains of uncounted centuries have since fallen, and the ice and the waters have worn and carved them into the area of distinguished beauty that is to-day the Glacier National Park.
But mark this: When the western edge of the earth's cracked skin overthrust the eastern edge, it brought its bottom surface over and on top of the eastern edge; and this bottom surface was the oldest sedimentary rock known, the very same strata of mud and limestone ooze which were deposited in the sea 80,000,000 years ago. And mark this, also, that the erosion of the years following has washed away all the deposits of the later geological ages that lay on the top of these strata, so that this ancient rock here lies fully exposed in all the glory of its greens and reds and grays, and all the fantastic carvings of the countless years. Of course the pressures which made the earth's skin rise and buckle and break made the Rocky Mountains, which at this point carry the Continental Divide. It is the same process which has made most of the mountain systems throughout the world, though there are few overthrusts so great as Glacier's.
The fantastic carving of Glacier National Park was principally the work of glaciers in the soft rock. Three times did great ice sheets, wooed south by falling temperatures, descend upon this region to dig the mighty cirques and scoop the immense valleys, and, between these visitations and since the last, frost and rain have chipped and washed and polished. Eating backward into the rocks from both sides, the glaciers nearly met a thousand times, leaving a land of enormous hollows separated by gigantic walls twisting and winding in all directions.
By these processes during uncountable years nature has created and decorated this marvelously beautiful region for our enjoyment to-day.
SCENES OF EXQUISITE BEAUTY
To picture to yourselves this region, imagine a chain of very lofty mountains twisting about like a worm, spotted everywhere with snow fields and bearing glistening glaciers in sixty or more hollows. Imagine these mountains crumbled and broken on their east sides into precipices sometimes three or four thousand feet deep and flanked everywhere by castellated walls, lesser peaks, and tumbled mountain masses of smaller size in whose hollows lie the most beautiful lakes you have ever dreamed of.
Down from the Continental Divide descend 19 principal valleys, 7 on the east side and 12 on the west. Of course there are very many smaller valleys tributary to each of these larger valleys. Through these valleys run the rivers from the glaciers far up on the mountains.
PURCHASED FROM THE INDIANS
Many of these valleys are not yet thoroughly known. It is possible that some of them have never been even entered unless by Indians. The great Blackfeet Indian Reservation, one of the many tracts of land set apart for the Indians still remaining in this country, adjoins the Glacier National Park on the east. Northward the park adjoins the Waterton Lakes Park in Canada.
There are 250 known lakes. There may be small ones in the wilder parts which white men have not yet even seen.
This region was not visited by white men till 1853, when a Government engineer, exploring for a route to the Pacific Ocean, ascended one of the creeks by mistake and returned when he found that no railroad could be built there. The next explorers were engineers who went in to establish the Canadian boundary line in 1861.
In 1890 copper was found and there was a rush of prospectors. In 1896 Congress bought the land east of the Continental Divide from the Blackfeet Indians, but there was not enough copper to pay for the mining. Since then few persons went there but big game hunters till 1910, when it was made a national park.
There are now several excellent hotels and several camps on the east side. The west side is wonderfully beautiful, too, and a hotel and camps are found there also.
There are a few good roads for automobiles and many miles of trail for walking and horseback riding. A railroad touches its southern boundary.
Last Updated: 30-Oct-2009