[Illustration: GLACIERS ON MOUNT TACOMA.]
Each succeeding autumn, for years past, has found me in some range of mountains, camping, hunting, fishing, climbing, and taking views. The benefits I have derived from these expeditions, in the way of health, strength, and vigor, are incalculable, and the pleasures inexpressible. My last outing was in the Cascade Range, in Oregon and Washington Territory, where I spent a month in these delightful occupations, and it is with a view of encouraging and promoting a love for these modes of recreation that this record is written.
"I live not in myself, but I become Portion of that around me; and to me High mountains are a feeling, but the hum Of human cities torture."
The Cascade Range of mountains extends from Southern Oregon through Washington Territory, away to the northward in British Columbia. In width, from east to west, it varies from fifty to one hundred miles. It is the most densely-timbered range on the continent, and yet is one of the highest and most rugged. It may not possess so many ragged, shapeless crags and dark cañons as the Rocky Range, and yet everyone who has ever traversed both accords to the Cascades the distinction of being the equal, in picturesqueness and grandeur, of the Rockies, or, in fact, of any other range in the country. As continental landmarks, Mounts Pitt, Union, Thielson, Jefferson, Hood, Adams, St. Helens, Tacoma, Baker, Stuart, Chiam, Douglass, and others are unsurpassed. Their hoary crests tower to such majestic heights as to be visible, in some instances, hundreds of miles, and their many glaciers feed mighty rivers upon whose bosoms the commerce of nations is borne. Mount Jefferson is 9,020 feet high; Mount Adams, 9,570; Mount St. Helens, 9,750; Mount Baker, 10,800, Mount Hood, 11,025, and Mount Tacoma, 14,444. There are many other peaks that rise to altitudes of 7,000 to 9,000 feet, and from these figures one may readily form something of an idea of the general height and beauty of the Cascade Range. The foot-hills are generally high, rolling, and picturesque, and so heavily timbered that in many places one cannot see a hundred yards in any direction. Higher up the range, however, this heavy timber is replaced by smaller trees, that stand farther apart, and the growth of underbrush is not so dense; consequently, the labor of travel is lightened and the range of vision is extended. The geological formation in the Cascades is varied. Igneous rock abounds; extensive basaltic cliffs and large bodies of granite, limestone, sandstone, etc., are frequently met with, and nearly all the table-lands, in and about the foot-hills, are composed of gravel drift, covered with vegetable mold. The Cascades may be explored with comfort later in the fall than the Rockies or other more eastern ranges, the winter setting in on the former much later than on the latter, although the winter rains usually come in November. September and October are the most pleasant months for an outing in the Cascades.