|Elevation||7,962 ft (2,427 m)|
|Parent range||Pacific Coast Ranges|
The Olympic Mountains are a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high – Mount Olympus is the highest at 7,962 ft (2,427 m); however, the eastern slopes rise out of Puget Sound from sea level and the western slopes are separated from the Pacific Ocean by the low-lying 20 to 35 km (12 to 22 mi) wide Pacific Ocean coastal plain. The western slopes are the wettest place in the 48 contiguous states. Most of the mountains are protected within the bounds of the Olympic National Park.
The mountains are spread out across four counties: Clallam, Grays Harbor, Jefferson and Mason. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
The Olympics have the form of a cluster of steep-sided peaks surrounded by heavily forested foothills and incised by deep valleys. They are surrounded by water on three sides, separated from the Pacific by the 20 to 35 km (12 to 22 mi) wide coastal plain. The general form of the range is more or less circular, or somewhat horseshoe-shaped, and the drainage pattern is radial.
Rivers radiate outwards to all sides. Clockwise from windward to leeward, the major watersheds are: Wynoochee, Humptulips, Quinault, Queets, Hoh, Bogachiel (all flowing into the Pacific; the Wynoochee by way of the Chehalis River, and the Humptulips by way of Grays Harbor), Lyre, Elwha, Dungeness (all flowing into the Strait of Juan de Fuca), Big Quilcene, Dosewallips, Duckabush, Hamma Hamma, and Skokomish (all flowing into Hood Canal).
The national park is surrounded on the south, east, and northwest sides by the Olympic National Forest, with five wilderness areas, and on the southwest side by the Clearwater State Forest with one Natural Area Preserve (Washington Department of Natural Resources), and the Quinault Indian Reservation. State parks and wildlife areas occur in the lower elevations.
Precipitation varies greatly throughout the range, from the wet western slopes to the arid eastern ridges. Mount Olympus, nearly 8,000 feet (2,400 m) tall, is a mere 35 miles (56 km) from the Pacific Ocean, one of the steepest reliefs globally and accounting for the high precipitation of the area, as much as 240 inches (6,100 mm) of snow and rain on Mount Olympus. 140 to 170 inches (3,600 to 4,300 mm) of rain falls on the Hoh Rainforest annually, receiving the most precipitation of anywhere in the continental United States. Areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Annual precipitation increases to about 30 in (760 mm) on the edges of the rain shadow around Port Townsend, the San Juan Islands, and Everett. 80% of precipitation falls during the winter. On the coastal plain, the winter temperature stays between −2 to 7 °C (28 to 45 °F). During the summer it warms up to stay between 10 and 24 °C (50 and 75 °F).
As a consequence of the high precipitation is the large number of snowfields and glaciers, reaching down to 1,500 m (5,000 ft) above sea level. There are about 184 glaciers crowning the Olympics peaks. The most prominent glaciers are those on Mount Olympus covering approximately 10 square miles (26 km2). Beyond the Olympic complex are the glaciers of Mount Carrie, the Bailey Range, Mount Christie, and Mount Anderson.
The Olympics are made up of obducted clastic wedge material and oceanic crust. They are primarily Eocene sandstones, turbidites, and basaltic oceanic crust. Unlike the Cascades, the Olympic Mountains are not volcanic, and contain no granite.
Millions of years ago, vents and fissures opened under the Pacific Ocean and lava flowed forth, creating huge underwater mountains and ranges called seamounts. The Farallon tectonic plate that formed a part of the Pacific Ocean floor (separate from the Pacific plate) inched eastward toward North America about 35 million years ago and most of the sea floor subducted beneath the continental land mass of the North America plate. Some of the sea floor, however, was scraped off and jammed against the mainland, creating the dome that was the forerunner of today's Olympics. In this particular case, the future Olympics were being jammed into a corner created by the Vancouver Island and North Cascades microcontinents attached to the western edge of the North America plate. This is thought to be the origin of the curved shape of the Olympic Basaltic Horseshoe, an arc of basalt running east along the Strait of Juan de Fuca, south along Hood Canal, and then west to Lake Quinault. Thrust-faulting northeast into the Vancouver Island/North Cascades corner pushes Olympic rock upward and southwestward, resulting in strata that appear to be standing on edge and that intermix with strata of different mineral composition. All this occurred under water; the Olympics began to rise above the sea only 10–20 million years ago.
The Olympics were shaped in the Pleistocene era by both alpine and continental glaciers advancing and retreating multiple times. The valleys of the Hoh, Queets, and Quinault rivers are typical U-shaped valleys carved by advancing alpine glaciers. Piles of talus and rockfall were created by retreating alpine glaciers. In the high mountains, the major rivers have their headwaters in alpine glacially carved cirques. During the Orting, followed by the Stuck, the Salmon Springs, and the Fraser glaciations, the vast continental Cordilleran ice sheet descended from Alaska south through British Columbia to the Olympics. The ice split into the Juan de Fuca and Puget ice lobes, as they encountered the resistant Olympic Mountains, carving out the current waterways and advanced as far south as present day Olympia. Ice flowed up the river valleys as far as 3,800 feet (1,200 m), carrying granitic glacial erratics with it.
The mountains support a variety of different ecosystems, varying by elevation and relative east-west location, which influences the local climate, primarily precipitation.
Olympic forests are coniferous forests, unique among mesic temperate forests in their almost complete dominance by conifers rather than by hardwoods. The hardwood:conifer timber volume ratio is 1:1,000 in the maritime Pacific Northwest. Another unique feature of Olympic forests is the size and longevity of the dominant tree species. Every coniferous genus represented here is represented by its largest and longest-lived species, and some of its second and third ranked species as well. Biomass accumulations are among the highest in the temperate forest zones. Dominance of conifers is thought to be a result of the amount and timing of precipitation. The dry summers limit the growth of deciduous trees, such as most hardwoods. Evergreens, such as most conifers, are able to take advantage of the winter precipitation by continuing to photosynthesize through fall, winter and early spring, when deciduous trees are not able to photosynthesize. No deciduous conifers occur in the Olympics; larch trees occur in the much-drier eastern Cascades, but not in the Olympics or western Cascades. There is only one species of evergreen hardwood, the madrone. The great size and age of conifers here is thought to be a result of the relative lack of frequent windstorms like tropical cyclones.
Along the western flanks of the mountains the increased orographic precipitation supports temperate rain forests in the Quinault, Queets, Hoh, and Bogachiel river valleys at low elevations. Protection by Olympic National Park, has allowed these rain forests to retain old growth trees, which supports a varied ecosystem. The Olympic rain forests are composed primarily of Sitka spruce and western hemlock, as are the surrounding lowland Sitka spruce forests, but are distinct in having a relative abundance of groves of bigleaf maple and vine maple, which support large epiphytic communities of mosses, lichens, ferns, and clubmosses; an abundance of nurse logs on the forest floor; a relatively open forest canopy and sparse shrub layer; and a dense moss layer on the forest floor. The rain forests are the wintering grounds for herds of Roosevelt elk and it is thought that browsing by the elk is responsible for the open shrub layer and the dominance of Sitka spruce over western hemlock.
The rain forests are just one type of forest found in the Olympic Mountains. Franklin and Dyrness  set out 5 forest zones: Sitka spruce, western hemlock, silver fir, mountain hemlock, and subalpine parkland. Other authors include a sixth, Douglas-fir zone. Different plant associations are typical of one or more forest zones. For instance, the rain forest plant association described above is a member of the Sitka spruce forest zone.
The Sitka spruce zone is a lowland zone dominated by Sitka spruce and western hemlock. Precipitation is high, winters are mild, elevations are low. This forest zone is typically found at very low elevations on the western coastal plain and not in mountainous areas, although it can be found as high as 1,900 feet (580 m).
The lower elevations of the Olympic mountains, from roughly 480 feet (150 m) up to 1,800 feet (550 m) – 3,700 feet (1,100 m), feature the western hemlock zone, so-called because in most of the zone, the climax tree species would be western hemlock, even though much of the area is dominated by Douglas-fir. The reason for this is that Douglas-fir is an early seral species, and reproduces primarily after disturbances such as fire, logging, landslides, and windstorms. Western hemlock does not reproduce well on disturbed, exposed soil but germinates under the canopy of Douglas-fir, eventually overtaking the forest by shading out the Douglas-fir, which cannot reproduce in shade. In this zone, despite the high annual precipitation, drought stress in summer is sufficiently severe to limit growth of many species, such as Sitka spruce. Hardwoods such as bigleaf maple, willows, and red alder are limited to disturbed sites and riparian areas. red-cedar grows in the wettest sites. A very small area of the northeastern rain shadow contains the limited Douglas-fir zone, where it is too dry for western hemlock.
Moving up in elevation and moisture availability is the silver fir zone, up to about 3,900 feet (1,200 m). This zone gets more precipitation, and more of it as snow, than the lower, warmer, drier western hemlock zone. The cold and the snowpack combine to limit growth of lower-elevation plants. On the other hand, silver fir is less drought tolerant and less fire tolerant than either Douglas-fir or western hemlock. Slide alder (Alnus viridis sinuata) grows in snow-creep areas and avalanche chutes, along with yellow-cedar. Meadows of thimbleberry also grow in this zone, often intergrading between the slide alder chutes and the silver fir forest.
The next higher forest zone is the mountain hemlock zone, the highest forest zone in the Olympic mountains. In this zone most precipitation falls as snow and the snow-free growing season is very short. In the drier rainshadow side of the mountains, mountain hemlock is largely replaced by subalpine fir. At the higher elevations of the mountain hemlock/subalpine fir zone, tree cover is reduced to isolated stands of trees called tree islands, surrounded by subalpine meadows, in the subalpine parkland zone. Variations in substrate, topography, moisture, and snowpack depth and duration determine the vegetation community. Tree islands form on convex topography, which tends to gather less snow and shed it sooner than surrounding level or concave topography.
In the west, the subalpine zone is dominated by mountain hemlock. It occurs along with subalpine fir from 1,100 to 1,650 metres (3,610 to 5,410 ft) in the Bailey Range; however, the range of this forest type is not extensive and does not extend much west of Mount Olympus, nor is it common in the east. Chamaecyparis nootkatensis|Yellow-cedar is sometimes found in relation to these plants. In the east and other drier areas, the subalpine zone is dominated by subalpine fir. It can occur with other trees, including mountain hemlock, silver fir, and yellow-cedar, but what characterizes these zones is the dominance of subalpine fir. These forests occur on the eastern ridges from 1,300 to 1,800 metres (4,300 to 5,900 ft).
In the Olympics, the treeline is between 5,000 feet (1,500 m) and 6,000 feet (1,800 m) but can be as low as under 4,000 feet (1,200 m) in some places. Treeline is a function of both elevation and precipitation, particularly the amount of snow that falls each winter. The growing season for trees is relatively short in the higher elevations of the windward Olympics, compared to similar elevations in other mountain ranges, due to the large accumulations of snow that take a long time to melt each year.
Subalpine meadows in the Olympic mountains are of 5 types. Heath shrub meadows are dominated by ericaceous huckleberries and heathers. Lush herbaceous meadows are typified by Sitka valerian and showy sedge. Drier areas or those with longer snow cover grow dwarf sedge (Carex nigricans) or grass (Festuca viridis) meadows. Phlox diffusa typifies the low herbaceous meadows of pumice, talus and scree slopes and other rocky areas. American saw-wort is common in both mountain meadows and lower subalpine parklands in the Olympics.
Above timberline is the Alpine zone, not a forest zone since no trees can grow this high. The alpine zone in the Olympics is much more limited in size than in other temperate mountain ranges, from 1,800 metres (5,900 ft) to 2,250 metres (7,380 ft). The high precipitation of the Olympics creates permanent snow and ice at lower elevations than is typical for other mountain ranges, cutting off the alpine vegetation zone. Most of the alpine vegetation is on the rain shadow side, in the northeastern Olympics, where there is less permanent snow and ice. Alpine vegetation is low herbaceous, typified by Phlox diffusa and species of Carex. Many of the Olympic Mountain’s endemic plants occur here, such as Piper’s bellflower (Campanula piperi) and Olympic violet (Viola flettii).
Mammals extirpated from the Olympic Mountains are the fisher (Martes pennanti) and the gray wolf (Canis lupus). The fisher was declared extirpated from Washington State when no fishers were detected during statewide carnivore surveys in the 1990s and 2000s. A reintroduction project was initiated in 2007, in partnership with Olympic National Park. The gray wolf was extirpated from Washington State in the early 20th century. The last wolf documented in the Olympics was trapped in 1920. In the early 21st century, wolves are naturally migrating back into eastern and north-central Washington State, but there is no evidence of wolf migration into the Olympics and no plan to translocate wolves to the Olympics.
Previous to the extirpation of the gray wolf, coyotes (Canis latrans) occurred in the lowlands of the Olympic peninsula but not in the mountains. With the absence of wolves, coyotes have been moving up into the higher elevations of the mountains and may be responsible for population declines in the Olympic marmot.
The mountain goat (Oreamnos americanus) is not native to the Olympic Mountains but was introduced for hunting in the 1920s by a coalition of the Forest Service, the Clallam County Game Warden, and the State Game Commission. Mountain goats in the Olympics have been associated with damage to alpine vegetation and soil erosion, and have shown aggression towards people. In 1999, a mountain goat gored a hiker at the summit of Mt. Ellinor in Olympic National Forest, and in 2010, a mountain goat fatally gored a hiker on the Klahane Ridge trail in Olympic National Park. In 2012, the trail to Mt. Ellinor was closed in summer due to aggressive goats, re-opening in the fall.
Roosevelt elk Cervus canadensis roosevelti range along the Pacific coast from the Russian River to Vancouver Island. Olympic and Vancouver Island elk are some of the last pure Roosevelt elk herds left; those in the Cascades have mixed with Rocky Mountain elk. Olympic National Park has the largest population of Roosevelt elk in the world. Some herds spend winter in lowland valleys, summer in high country, in subalpine meadows. Other herds live year-round in lowland forests and meadows. Elk prefer more humid areas, the Sitka spruce, wet western hemlock, and mountain hemlock zones. Elk browsing is believed to be responsible for the open park-like structure of the Olympic rainforests; the elk graze on hemlock and shrubs, leaving the Sitka spruce to grow. Elk browsing also increases diversity of grasses and forbs. Elk exclosure experiments in rainforest valleys show more species of vegetation growing outside the exclosures, where elk browse, than inside; while there are more brush and saplings inside exclosures, there are more grasses and forbs outside. Elk browsing improves forage for other herbivores like deer, voles and snowshoe hares. Elk prefer old growth forest and young alder groves over the large, even-aged plantations common on commercial timber land, although they will use small, recent clearcuts where they mimic natural forest openings.
Both the Press and O’Neil expeditions were impressed by the quantity and tameness of the elk. to 4000 hunters came, several times as many as expected. One hunter was accidentally shot and died. A second hunter drowned in the Hoh River. A pack horse was shot. The Hoh River flooded, stranding hunters and washing away their camps. Forest Service and State Game personnel were overwhelmed with rescue efforts (lost, stranded, or injured hunters) and dispute resolution. Over 800 elk were killed, some left lying in the forest. Proponents of a national park used the 1937 elk hunt as an argument in favor of permanent protection for Olympic’s elk herds. Not all the elk herds are protected inside the national park. Some migrate in and out of the park, and others live entirely outside the park; these are subject to regulated hunting when not in the national park.
Blacktail deer (Odocoileus hemionus columbianus) prefer drier areas than elk, such as the dry western hemlock, Douglas-fir, and subalpine fir zones. Similar to the elk, blacktail deer winter in lowlands, or along south-facing ridges, and summer in the high country meadows.
Cougar (Felis concolor) is the largest carnivore in the Olympics. Their main prey are deer and elk but they also hunt porcupines and insects. They are rarely seen in the Olympics but are thought to be widespread and relatively common.
Banana slug (Ariolimax columbianus) is another Pacific Northwest endemic. Slugs are abundant in the Olympic forests, outweighing mammals and birds combined. They thrive in the cool damp shade of the forests. The banana slug is the largest and most conspicuous of Olympic slugs.
Northern spotted owl (Strix occidentalis caurina) is an old-growth dependent species and is listed as threatened under the Endangered Species Act. The majority of spotted owls on the Olympic peninsula, along with the largest preserve of temperate old-growth forest, live in the national park. Spotted owls prey on flying squirrels and snowshoe hares, and are themselves preyed on by great horned owls Bubo virginianus. The density of the canopy of an old-growth forest gives the spotted owls some protection from the larger, less agile great horned owls.
Rufous hummingbird (Selasphorus rufus) is the only hummingbird in the Olympics. They overwinter in Mexico and southern California, arriving in the Olympics in February or March with the flowering of the Indian plum Oemleria cerasifera.
Osprey (Pandion haliaetus) and bald eagle (Haliaeetus leucocephalus) fish in Olympic rivers, nesting in large old trees. Both are relatively common, the bald eagle more so along the coast than in the mountains.
Olympic rivers are dominated by Pacific salmonids, the Oncorhynchus. Chinook, coho, pink, rainbow and steelhead, and cutthroat all spawn in Olympic rivers. Chum and sockeye also live in coastal Olympic peninsula rivers but do not reach into the mountains. Bull trout (Salvelinus confluentus) and Dolly Varden trout (S. malma) also live in Olympic rivers.
Near-endemics, those that occur in the Olympics as well as other parts of a limited range, include the Cope's giant salamander (Dicamptodon copei), and the Van Dyke's salamander (Plethodon vandykei,) both found primarily in the Olympics and other mountainous areas of western Washington; the tailed frog (Ascaphus truei), of Pacific Northwest mountain streams, and the mountain beaver (Aplodontia rufa) of the coastal Pacific Northwest.
For the original inhabitants of the Olympic Peninsula, the highest peaks of the mountains were the only refuges during the Great Floods at the beginning of time.
Archeological evidence shows that the Olympic Mountains were inhabited by Paleolithic hunters after the retreat of the Cordilleran Ice Sheet. Stone tools in the Deer Park area date to 7600 years ago, prior to the volcanic eruption of Mount Mazama. Similar tools have been found near Lake Cushman and throughout the Olympic subalpine meadows and ridges, as well as in coastal areas. In addition, a fragment of a woven basket found in the Olympic subalpine of Obstruction Point was radiocarbon dated to nearly 3000 years ago.
The mountains were originally called "Sun-a-do" by the Duwamish Indians, while the first European to see them, the Spanish navigator Juan Pérez, named Mount Olympus "Santa Rosalia", in 1774. But the English captain John Meares, seeing them in 1788, thought he would honor the Greek explorer Juan de Fuca who claimed to have found the fabled Northwest passage nearby by naming the mountain after the mythical home of Greek Gods which is "Mount Olympus" in Greece. Various names for the mountains were used based on the name Mount Olympus, including the Olympic Range, the Olympian Mountains, and the Olympus Range. Alternate proposals never caught on, and in 1864 the Seattle Weekly Gazette persuaded the government to make the present-day name official, although other names continued to be used.
Though readily visible from many parts of western Washington, especially Seattle, the interior was almost entirely unexplored until 1885, when 2nd Lt. Joseph P. O'Neil of the 14th Infantry, stationed at Fort Vancouver, led a small expedition into the northern Olympics from Port Angeles.
In late 1889, Charles A. Gilman and his son Samuel explored the East Fork Quinault up to its headwaters, but chose to return the way they came rather than cross over the mountains.
The first crossing of the Olympic Mountains was done from November 1889 through May 1890 by the Press Expedition, a group of 5 men led by Canadian James H. Christie, sponsored by the Seattle newspaper Press, which ascended the Elwha River and descended the North Fork Quinault River. The Press party included 2 mules, which both died in separate incidents, and 4 dogs, 1 of which was killed by an elk.
Once on the mainstem Quinault River, the men built a raft, but it wrecked on a logjam. The settler and neighboring Indians took the expedition across Lake Quinault and down the lower river to the coast in mid May, nearly six months after they left Port Angeles.
O'Neil returned to Washington in 1887 and started planning another expedition. This expedition was larger than the 1885 expedition, and would be resupplied by mule train from Hoodsport on Hood Canal, allowing time for scientific exploration of the area. The expedition consisted of 10 soldiers, 1 civilian mule packer, 4 civilian scientists from the Oregon Alpine Club, 11 mules, 1 bell mare to lead the mule train, and up to 4 dogs. The scientists collected specimens of plants, animals, and minerals, which they shipped back to Portland by way of the mule train to Hoodsport. The majority of the party was assigned to cutting the mule trail, while 2 or 3 man exploring parties fanned out and scouts went ahead. The scouts and side exploring parties scrambled up slopes on all fours, pulling themselves up by grabbing onto vegetation; descended similar slopes by sliding, deliberately or inadvertently; hacked and crawled through dense brush and windthrow; waded up rivers and streams when there was no other way through; felled trees to bridge ravines and rivers; and traversed narrow ridges of crumbling vertically-oriented shale. Hornet and yellow jacket wasp attacks were a daily occurrence, sending men scrambling and mules stampeding, one over a cliff to her death. Where the men crossed swamps, devils club thorns impaled the men and broke off in their skin, creating painful inflammations.
Once camped in the central mountains, O’Neil sent out small exploring parties to the Duckabush, Dosewallips, South Fork Skokomish, Wynoochee and Humptulips rivers, and to Mount Olympus and the Queets River. One party of 3 men climbed what they thought was Mount Olympus but was in reality one of the neighboring peaks, Athena II. A fourth member of the summit party became separated on the climb and ended up descending the Queets River alone, and was taken in by a Quinault Indian family. They were reluctant to believe that he had crossed the Olympics, not believing it was possible to do so; but they accepted his story when he was able to point out reference points on a map. (Many members of this expedition spoke Chinook jargon.) From their settlement, he was able to rejoin the expedition in Hoquiam. O'Neil's reports on his explorations resulted in his recommendation that the region be declared a national park.
Mount Olympus itself was not ascended until 1907, one of the first successes of The Mountaineers, which had been organized in Seattle just a few years earlier. A number of the more obscure and least-accessible peaks in the range were not ascended until the 1970s.
President Grover Cleveland protected the forests of the Olympic Peninsula with the Olympic Forest Reserve in 1897. Initially the reserve consisted of over 2 million acres, nearly the entire peninsula. Forest Service surveyors Dodwell and Rixon spent three years surveying, timber cruising, and mapping the new reserve. Their report, published in 1902, reported that most of the land was not suited to agriculture, but local politicians had already convinced President William McKinley to remove the most valuable lowland timber from the reserve, claiming it should be open to homesteading. Private timber companies paid ‘homesteaders’ to file claims on land that they then sold to the timber company. At the same time, commercial hunters reduced the Olympic elk herds to fewer than 2000 animals, prompting the state legislature to impose a temporary moratorium on elk hunting in the Olympics. The Forest Reserve was reorganized under Gifford Pinchot as the Olympic National Forest in 1905, with an emphasis on commercial utilization of timber and minerals and fire protection, as well as hunting and trapping. With the passing of the Antiquities Act in 1906, which allowed the president to designate national monuments, Mount Olympus National Monument, administered by the Forest Service, was proclaimed by Theodore Roosevelt in 1909 in order to protect the elk herds. In 1914, the new supervisor of the Forest Service, Henry Graves, made a trip to the Olympics to determine if commercial timber and minerals were being tied up in the national monument. As a result of Grave’s report, President Woodrow Wilson removed a third of a million acres from the monument.
The Elwha River was dammed in 1910 with construction of the Elwha Dam. A second dam was built a few miles upstream in 1927. Neither dam had any fish passage for the salmonid runs, completely eliminating salmonids from over 70 miles of river. Congress authorized removal of these dams in 1992, and work began in 2011.
The North Fork Skokomish River was dammed in the 1920s by the city of Tacoma, enlarging the original Lake Cushman by 600%. A settlement was reached in 2009 with the Skokomish Indian Tribe over damages to fisheries and game habitat, damages to tribal lands through flooding, and trespass on tribal lands for the power transmission line. As part of the settlement, migrating salmon will be trucked around the dam.
The Wynoochee River was dammed in the late 1960s by the Army Corps of Engineers for flood control, but in 1994 the dam was taken over by the city of Tacoma for power generation. Migrating salmon are trucked around the dam, and Tacoma Public Utilities funds mitigation for Roosevelt elk wintering habitat that was lost under the reservoir.
With the building of the Spruce Railroad during World War I and the completion of the Olympic Highway in 1931, logging in the Olympics intensified, along with demand for recreational facilities. During this period the Forest Service built roads and campgrounds and encouraged private businesses with special use permits to build tourist facilities such as a winter sports facility at Deer Park and the chalets in Enchanted Valley and at Low Divide. Special use permits were also issued for private summer cabins at Lakes Cushman and Quinault, and the Olympic Hot Springs resort. During the Great Depression, the Olympic National Forest used the Civilian Conservation Corps to build logging roads and railroads, bridges, campgrounds, shelters, fire lookouts, ranger stations, and a fish hatchery. They also fought fires and planted tree seedlings.
Pressure for a national park built with the acceleration of logging and road building. The Forest Service campaigned in peninsula logging and mill towns against the national park, and both the Forest Service and the Park Service jockeyed for public support and endorsement from various conservation groups for administration of the monument. In 1935, a special committee was convened on the national park proposal. The majority reported that the Olympics fully rated protection as a national park, but one member issued a minority report stating that public pressure for recreational facilities would require the Park Service to build roads, campgrounds, and chalets, thus negating any benefit from national park status. Both the Forest Service and the Park Service sponsored backcountry trips through the high Olympics that summer to promote their stewardship of the mountains.
In 1937, President Franklin D. Roosevelt visited the Olympics to determine their suitability as a national park, and was greeted in Port Angeles by more than 3000 local school children asking him to ‘give us our Olympic National Park’. He signed Olympic National Park into law in 1938. In 1953, the park was enlarged with the addition of the coastal strip, and more coastal areas along Lake Ozette were added in 1976. Also that year, UNESCO named the park an International Biosphere Reserve, and a World Heritage Site in 1981. In 1984, Congress designated 5 wilderness areas in the Olympic National Forest, and declared 95% of Olympic National Park a wilderness area in 1988.
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