The National Park System, of which this park is a unit, is dedicated to conserving the scenic, scientific, and historic heritage of the United States for the benefit and enjoyment of its people.
A superintendent, whose address is 600 East Park Avenue, Port Angeles, Wash., 98362, is in immediate charge of the park.
America’s Natural Resources
Created in 1849, the Department of the Interior—America’s Department of Natural Resources—is concerned with the management, conservation, and development of the Nation’s water, wildlife, mineral, forest, and park and recreational resources. It also has major responsibilities for Indian and territorial affairs.
As the Nation’s principal conservation agency, the Department works to assure that nonrenewable resources are developed and used wisely, that park and recreational resources are conserved, and that renewable resources make their full contribution to the progress, prosperity, and security of the United States—now and in the future.
Contents
PAGE [THE MOUNTAINS ARE FORMED] 2 [GLACIATION] 5 [THE SHAPE OF THE LAND TODAY] 5 [GLACIERS TODAY] 6 [CLIMATE AND THE WATER CYCLE] 9 [THE FORESTS AND WILDFLOWERS] 11 [Rain Forest] 13 [Mountain Vegetation] 16 [HOW TO IDENTIFY SOME COMMON PLANTS] 23 [Trees] 23 [Shrubs] 27 [Nonwoody Plants] 28 [WILDLIFE] 35 [You and the Animals] 36 [Seeing the Mammals] 37 [Birds] 42 [Fish] 46 [Other Animal Life] 47 [PACIFIC COAST AREA] 48 [MAN IN OLYMPIC] 51 [Indians of the Olympic Peninsula] 51 [Exploration by sea] 52 [Exploration by land] 54 [Establishment of the Park] 56 [SUGGESTED READINGS] 57
Here is truly a living wilderness nurtured by the ocean! The Olympic Mountains stand first in line against the moisture-filled Pacific winds. These winds, rising and cooling on the western slopes, drop 12 to 18 feet of rain and snow on forest and mountain each year. Two extraordinary conditions result—a temperate-climate rain forest and an abundance of permanent ice bodies at comparatively low altitudes. Many rushing streams return the water from snowfields, glaciers, and forest slopes to the sea. A complete and endless circuit of water from ocean to land and back to the ocean may be observed from a single mountain vantage point. One can hardly fail to notice a water cycle of this magnitude and completeness or to appreciate its great influence on the Olympic scene.
Olympic rocks tell of their having been formed of mud, sand, and lava, uplifted from the sea; they tell of earth disturbance that alternately submerged the land beneath the sea and elevated it into mountains. The rocks and the shape of the land also tell of colder climates, when ice from the north made almost a glacier island of the Olympic Mountains, and of mountain valley glaciers which sculptured the mountains during thousands of years. The rugged beauty of the Olympic high country, enhanced by scores of mountain lakes, bears testimony to the former presence of these extensive glaciers.