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The wooden flume has a cross section of 8 by 8 feet (2.4 by 2.4 m) and can supply up to 400 cubic feet (11 m 3) of water per second to the turbines of the Electron powerhouse. [2] Original construction took approximately 14 months to complete. The grade is uniform and runs at seven feet of elevation per mile.
The Edith Creek Chlorination House is a historic structure in Mount Rainier National Park, built by the National Park Service in 1930. The rustic structure was built as part of the water supply system to the Paradise area. The low concrete building with stone veneer cladding was built to withstand very heavy snow loads.
At Auburn, the Green River emerges from the Green River Valley and enters the much larger Auburn/Kent Valley, which was created by glacial action during the Pleistocene ice ages, then filled in by river sediments and lahars from Mount Rainier. After flowing generally west from its source, at Auburn the river turns north, entering a zone of ...
Mount Rainier is the tallest mountain in Washington and the Cascade Range. This peak is located southeast of Tacoma, approximately 60 miles (97 km) south-southeast of Seattle. [26] [27] Mount Rainier has a topographic prominence of 13,210 ft (4,026 m). [2]
The dry gravel bed of the White River floodplain near the campground in Mount Rainier National Park. The source of the White River is the Emmons Glacier on the northeast side of Mount Rainier. The river flows from ice caves at the toe of the glacier. Its upper reach is contained within Mount Rainier National Park. Shortly after emerging from ...
Detailed map of Mount Rainier's summit and northeast slope showing upper perimeter of Osceola collapse amphitheater (hachured line) The Osceola Mudflow, also known as the Osceola Lahar, was a debris flow and lahar in the U.S. state of Washington that descended from the summit and northeast slope of Mount Rainier, a volcano in the Cascade Range during a period of eruptions about 5,600 years ago.
The two streams flow through the western part of Mount Rainier National Park, joining just outside the park boundary and forming the Puyallup River proper. The main Puyallup River flows north and northwest from Mount Rainier. The tributary Mowich River, which also flows from glaciers on Mount Rainier, joins the Puyallup from the east. Below the ...
The Longmire Historic District is in turn part of the Mount Rainier National Historic Landmark District, which encompasses the entire park and which recognizes the park's inventory of Park Service-designed rustic architecture. [1] Longmire is the second most popular destination for visitors to Mount Rainier National Park after Paradise.