Post 22418
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The big game which formerly ranged this peak included buffalo, deer, elk, mountain sheep, the grizzly, the black bear, the mountain lion, the fox, the coyote, and the wolf. Along the descending streams, through one vertical mile of altitude, were beaver colonies, terrace upon terrace. No one knows how many varieties of wild flowers each year bloom in all the Peak’s various ragged zones, but there are probably no fewer than two thousand. Along with these are a number of species of trees. Covering the lower part of the mountain are growths of cottonwood, Douglas spruce, yellow pine, white fir, silver spruce, and the Rocky Mountain birch. Among the flowering plants are the columbine, shooting-star, monkshood, yucca or Spanish bayonet, and iris. Ascending, one finds the wintergreen, a number of varieties of polemonium, the paintbrush, the Northern gentian, the Western yarrow, and the mertensia. At timber-line, at the altitude of about eleven thousand five hundred feet, are Engelmann spruce, arctic willow, mountain birch, foxtail pine, and aspen. At timber-line, too, are the columbine, the paintbrush, and a number of species of phlox. There are no trees in the zone which drapes the uppermost two thousand feet of the summit, but in this are bright flowers,–cushion pinks, the spring beauty, the alpine gentian, the mountain buckwheat, the white and yellow mountain avens, the arctic harebell, the marsh-marigold, the stonecrop, and the forget-me-not. One summer I found a few flowers on the summit.
Isolation probably rendered the summit of this peak less favorable for snow-accumulation during the Ice Age than the summits of unisolated peaks of equal altitude. During the last ice epoch, however, it carried glaciers, and some of these extended down the slopes three miles or farther. These degraded the upper slopes, moved this excavated material toward the bottom, and spread it in a number of places. There are five distinct cuplike hollows or depressions in this peak that were gouged by glaciers. The one lying between Cameron’s Cone and the summit is known as the “Crater.” A part of this is readily seen from Colorado Springs. Far up the slopes are Lake Moraine and Seven Lakes, all of glacial origin.
The mountain mass which culminates in Pike’s Peak probably originated as a vast uplift. Internal forces appear to have severed this mass from its surroundings and slowly upraised it seven thousand or more feet. The slow uprising probably ended thousands of years ago. Since that time, disintegration, frost, air, and stream erosion have combined to sculpture this great peak. Pike’s Peak might well be made a National Park.