'Mount Rainier National Park' is a
United States National Park located in southeast
Pierce County and northwest
Lewis County in
Washington state.
[1] It was established on
March 2, 1899, the fifth national park in the United States. The park contains including all of
Mount Rainier, a 14,410-foot (4,392 m)
stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet (490 m) to over 14,000 feet (4,300 m). The highest point in the
Cascade Range, around it are valleys, waterfalls, subalpine wildflower meadows, old growth forest and more than 26
glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.
Mount Rainier is circled by the
Wonderland Trail and is covered by several glaciers and snowfields totaling some .
Carbon Glacier is the largest glacier by volume in the
continental United States, while
Emmons Glacier is the largest glacier by area. About 1.3 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for
mountain climbing with some 10,000 attempts per year with approximately 25% making it to the summit.
The park contains outstanding examples of
old growth forests and
subalpine meadows.
History
Ninety-seven percent of the park is preserved as
wilderness under the
National Wilderness Preservation System, including
Clearwater Wilderness, a designation it received in 1988. It is abutted by the
Tatoosh Wilderness. The park was designated a
National Historic Landmark on
February 18, 1997 as a showcase for the
National Park Service Rustic style architecture (or ''parkitecture'') of the 1920s and 1930s, exemplified by the
Paradise Inn and a masterpiece of early NPS master planning. As an Historic Landmark district, the park was administratively listed on the
National Register of Historic Places.
Native Americans
The earliest evidence of human activity in the area which is now Mount Rainier National Park is a projectile point dated to circa 4,000-5,800 BP (
before present) found along Bench Lake Trail (the first section of Snow Lake Trail).
Part One: The Cultural Setting. I. Historical Overview Of Indians And Mount Rainier
Chapter 4:
The 1995 Mount Rainier Archeological Reconnaissance
A more substantial archeological find was a rock shelter near Fryingpan Creek, east of Goat Island Mountain. Hunting artifacts were found in the shelter. The shelter would not have been used all year round. Cultural affinities suggest the site was used by
Columbia Plateau Tribes from 300 to 1,000 BP.
In 1963 the National Park Service contracted the
Washington State University to study
Native American use of the Mount Rainier area. Richard D. Daugherty lead an archeological study of the area and concluded that prehistoric humans used the area most heavily between 4,500 and 8,000 BP. Allan H. Smith interviewed elderly Native Americans and studied ethnographic literature. He found no evidence of permanent habilitation in the park area. The park was used for
hunting and gathering and for occasional
spirit quests. Smith also came to tentative concussions that the park was divided among five tribes along watershed boundaries; the
Nisqually,
Puyallup,
Muckleshoot,
Yakama, and
Taidnapam (Upper Cowlitz). Subsequent studies cast doubt on Smith theory that the tribes had agreed upon boundaries before they entered into treaties with the United States in 1854-55.
Major attractions
Paradise
Main articles: Paradise, Washington
'Paradise' (
[2])is the name of an area at approximately on the south slope of Mount Rainier in the national park. Paradise is the most popular destination for visitors to Mount Rainier National Park.
[3] 62% of the over 1.3 million people who visited the park in 2000 went to Paradise.
[4] Paradise is the location of the historic
Paradise Inn (built 1916),
[5] Paradise Guide House (built 1920) and
Henry M. Jackson Visitor Center (built 1966).
[6]
The
National Park Service says that "Paradise is the snowiest place on Earth where snowfall is measured regularly."
[7] 1,122 inches (93.5 ft, 28.5 m) of snow fell during the winter of 1971-1972, setting a world record for that year.
7[8] It also holds the Cascade Range record for most snow on the ground with 367 inches (9.3 m) on
March 10 1956.
[9].
Longmire
Main articles: Longmire

National Park Service 1928 Administration Building at Longmire
'Longmire' () is a
visitor center in Mount Rainier National Park, located east of the Nisqually Entrance. The area is in the
Nisqually River valley at an elevation of
[10] between The Ramparts Ridge and the Tatoosh Range. Longmire is surrounded by old-growth
douglas fir,
western red cedar and
western hemlock.
Longmire is the location of Mount Rainier's National Park Inn, the Longmire Museum, and the 1928 National Park Service Administration Building, which is now a Wilderness Information Center. The National Park Inn is the only accommodation in the park open all year round.
[11]
Longmire is the second most popular destination for visitors to Mount Rainier National Park after Paradise. Of the more than 1.3 million people who visited the park in 2000, 38% visited Longmire.
4 The Cougar Rock
Campgound is about north west of Longmire.
1 Longmire is one of the starting points of the
Wonderland Trail.
Sunrise

Subalpine meadows at Sunrise
'Sunrise' () is a
lodge and
visitor center located in the northeastern part of Mount Rainier National Park in
Pierce County,
Washington,
United States. At an elevation of 6,400 feet (1,950 m), it is the highest point in the park that is accessible by vehicle. There are
miles of trails located all around Sunrise, such as Mount Fremont and
Sourdough Ridge. The lodge is reachable via a 10 mile (16 km) turnoff from
WA 410 near the
White River entrance.
Flooding in November 2006
Mount Rainier National Park closed due to extensive flooding as a result of the
November 6,
2006 Pineapple Express rainstorm when of rain fell in a 36 hour period. Campsites and roads throughout the park were washed away. Power to Paradise and Longmire was disrupted.
[12] On
May 5,
2007, the park reopened to automobile traffic via
Washington State Route 706 at the Nisqually Entrance.
[13]
References
1.
2.
Coordinate measured using National Geographic TOPO! Software Version 3.4.3.
3.
Moon Handbooks Washington, , Don, Pitcher, Avalon Travel Publishing, ,
4.
Mount Rainier National Park Visitor Study Brochure
5.
6. Mt. Rainier National Park Centennial Timeline 1960s
7.
Mount Rainier National Park - Frequently Asked Questions (U.S. National Park Service)
8.
Annual Snowfall at Paradise 1920 to 2002
9.
Skiing the Cascade Volcanoes
10.
Discovering the Wonders of the Wonderland Trail: Encircling Mount Rainier (5th edition), Filley, Bette, , , Dunamis House, 2002, ISBN 1-880405-09-1
11.
12.
November 2006 Flooding
13.
Battered Mt. Rainier to reopen Debera Carlton Harrell
External links
★ Official site:
Mount Rainier National Park
★
Park map (PDF, 2 MB), provided by the
National Park Service
★
National Historic Landmark information
★
University of Washington Libraries Digital Collections – Rainier National Park Mountain-Glacier Wonderland Photograph Album 50 photographs from a promotional album (ca. 1925) for Mount Rainier National Park depicting tourist facilities, scenic views of the mountain and surrounding parkland, and recreational activities including mountaineering.
★
★
Electronic Documents outlining the natural and cultural history of the park, including the complete Nature Notes (newsletter) series and the park's Administrative History [National Park Service]