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 contiguous United States. 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. Precipitation varies greatly throughout the range, from the wet western slopes to the arid eastern ridges. State parks and wildlife areas occur in the lower elevations. 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. ![]() Of this portion, 95% is part of the Daniel J. Hurricane Ridge – road accessible summit near Port AngelesĪ large portion of the range is contained within the Olympic National Park.Mount Storm King – located just to the south of Lake Crescent.Boulder Peak – Peak located in the Lake Crescent and Elwha River area.The Brothers – double peak visible from Seattle.Mount Anderson – West Peak of Mount Anderson is the hydrographic apex of the Olympic Mountains: From this peak, rivers flow outward to the Pacific Ocean, the Strait of Juan de Fuca, and Hood Canal.Mount Townsend – highly visible from Seattle at far northeast of the Olympics (technically in the Buckhorn Wilderness).Mount Constance – largest peak visible from Seattle.Mount Olympus – highest point, eight glaciers.Mount Anderson as seen from the East Fork of the Quinault River Clockwise from windward to leeward, the major watersheds are: Satsop, Wynoochee, Humptulips, Quinault, Queets, Hoh, Bogachiel, Sol Duc (all flowing west into the Pacific Ocean with the Satsop and Wynoochee by way of the Chehalis River, and the Humptulips by way of Grays Harbor at the mouth of the Chehalis River), Lyre, Elwha, Dungeness (all flowing north into the Strait of Juan de Fuca), Big Quilcene, Dosewallips, Duckabush, Hamma Hamma, and Skokomish (all flowing east into Hood Canal). The general form of the range is more or less circular, or somewhat horseshoe-shaped, and the drainage pattern is radial. 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 Olympics have the form of a cluster of steep-sided peaks surrounded by heavily forested foothills and incised by deep valleys. ![]() ![]() The Brothers is the large double peak on the left, and Mount Constance is on the right. The Olympic Mountains in winter, as seen from the east. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System. The mountains are located in western Washington in the United States, spread out across four counties: Clallam, Grays Harbor, Jefferson and Mason. ![]() Most of the mountains are protected within the bounds of Olympic National Park and adjoining segments of the Olympic National Forest. The western slopes are the wettest place in the 48 contiguous states. The mountains, part of the Pacific Coast Ranges, are not especially high – Mount Olympus is the highest at 7,965 ft (2,428 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 Olympic Mountains are a mountain range on the Olympic Peninsula of the Pacific Northwest of the United States.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |