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Mount Rainier is a stratovolcano in the Cascade Volcanic Arc that consists of lava flows, debris flows, and pyroclastic ejecta and flows. Its early volcanic deposits are estimated at more than 840,000 years old and are part of the Lily Formation (about 2.9 million to 840,000 years ago).
Mount Rainier National Park is an American national park located in southeast Pierce County and northeast Lewis County in Washington state. [3] The park was established on March 2, 1899, as the fourth national park in the United States, preserving 236,381 acres (369.3 sq mi; 956.6 km 2) [1] including all of Mount Rainier, a 14,410-foot (4,390 m) stratovolcano.
The day before its 1980 eruption, Mount St. Helens was the fifth highest major summit of Washington. Today, Mount St. Helens is the 35th highest major summit of the state. This article comprises three sortable tables of major mountain peaks [1] of the U.S. State of Washington. The summit of a mountain or hill may be measured in three principal ...
Crystal Mountain is a mountain and alpine ski area in eastern Pierce County, Washington, United States, located in the Cascade Range southeast of Seattle. It is the largest ski resort in the state of Washington and lies within the Mount Baker–Snoqualmie National Forest. The resort is accessible from the Seattle– Tacoma metropolitan area via ...
Mineral Mountain is a 6,503 feet (1,982 m) mountain in Mount Rainier National Park, in Pierce County of Washington state. [4] It is part of the Cascade Range, and lies 5 mi (8.0 km) due north of the summit of Mount Rainier. The Wonderland Trail provides an approach to this mountain, and the summit offers views of Old Desolate and the Winthrop ...
Tatoosh Range. / 46.745°N 121.7°W / 46.745; -121.7. The Tatoosh Range is a mountain range located in Mount Rainier National Park and the adjacent Tatoosh Wilderness in the state of Washington, in the Pacific Northwest region of the United States. [1] The range runs roughly east–west, beginning with the southeastern Moon Mountain and ...
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.
From May 24 through Labor Day, most visitors entering the Nisqually and Stevens Canyon entrances between 7 a.m. and 3 p.m. will need to make an online or phone reservation ahead of time.