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Majestic Rainier

A comprehensive geological and volcanic profile of the prominent stratovolcano in Washington's Cascade Range.

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Name

Indigenous Nomenclature

Mount Rainier is known by numerous names in the languages of the Indigenous peoples who have inhabited the region for millennia. Linguistic analysis identifies names such as xสทaqฬ“xฬŒaqฬ“สทษ™sh ('sky wiper') and tษ™qสทubษ™ส” ('snow-covered mountain') in Lushootseed, and tษ™xสทqฬ“ษ™ma or tษ™qสทqฬ“ษ™ma in Cowlitz. These names reflect a deep cultural connection and observation of the mountain's prominent features.

European Naming

The mountain was officially named Mount Rainier in 1792 by Captain George Vancouver, in honor of his friend Rear Admiral Peter Rainier. This designation occurred during a period of European exploration and territorial claims in the Pacific Northwest. The name 'Tacoma', derived from Indigenous terms, was also used and favored by local residents for a period, leading to historical naming debates.

Official Designation

Despite the historical use of 'Tacoma', the United States Board on Geographic Names officially designated 'Rainier' as the mountain's name in 1890. Subsequent efforts to revert to or recognize Indigenous names have continued, reflecting evolving perspectives on historical nomenclature and cultural heritage.

Geography

Location and Prominence

Mount Rainier is situated in Washington State, approximately 95 km (59 miles) south-southeast of Seattle. It is the highest peak in the Cascade Range and the state of Washington. Its significant topographic prominence of 4,030 meters (13,210 feet) makes it the most prominent mountain in the contiguous United States.

Visibility

On clear days, Mount Rainier is a dominant feature visible from the Seattle-Tacoma metropolitan area and beyond. Its visibility can extend as far as Corvallis, Oregon, and the North Shore Mountains in British Columbia, underscoring its immense scale and presence in the regional landscape.

Hydrological Significance

The mountain serves as the source for several major rivers, including the Carbon, Cowlitz, Nisqually, Puyallup, and White Rivers. These glacial meltwater systems are vital for regional ecosystems and human use, including hydroelectric power generation and irrigation.

Subsidiary Peaks

Summit Features

Mount Rainier's summit plateau hosts three named summits. The highest is the Columbia Crest. Point Success, the second highest, is located at the southern edge, while Liberty Cap marks the northwestern edge, overlooking dramatic features like Willis Wall.

Little Tahoma Peak

To the east of the main summit lies Little Tahoma Peak, an eroded remnant of an earlier volcanic cone. With a prominence of 262 meters (858 feet), it is often considered a separate peak and, if so, would rank as the third highest mountain in Washington.

Height

Official Elevation

The officially recognized summit elevation of Mount Rainier at the Columbia Crest is 4,392 meters (14,410 feet) according to the National Park Service and USGS, based on the 1956 measurement referenced to the 1929 datum. A commonly cited alternative measurement is 4,392.5 meters (14,411 feet) based on the 1988 datum.

Recent Findings

Recent surveys conducted in 2024 suggest that glacial melt has altered the mountain's summit height. Preliminary findings indicate the Columbia Crest may now be at 4,385.8 meters (14,389.2 feet), while the Southwest Rim has been measured at 4,389.0 meters (14,399.6 feet), potentially making it the new highest point.

Geology

Volcanic Formation

Mount Rainier is a large, active stratovolcano formed by subduction zone volcanism within the Cascade Volcanic Arc. Its geological history spans approximately 500,000 years, with early volcanic deposits dating back over 840,000 years. The volcano is primarily composed of andesite lava flows, debris flows, and pyroclastic ejecta.

Lahars and Avalanches

The volcano's substantial glacial ice content makes it prone to generating massive lahars (volcanic mudflows) and debris avalanches. Significant past events include the Osceola Mudflow (approx. 5,000 years ago) and the Electron Mudflow (approx. 530-550 years ago), which reached far into the surrounding valleys and Puget Sound.

Geothermal Activity

Geothermal heat from within the volcano maintains snow-free areas on the crater rims and has formed the world's largest known network of glacier caves within the ice-filled craters. This internal heat also contributes to the hydrothermal activity that slowly weakens the volcano.

Volcanic Hazard

High-Risk Designation

Mount Rainier is classified as a Decade Volcano due to its high probability of future eruption and its proximity to densely populated areas. Its potential to produce catastrophic lahars poses a significant threat to communities in the Puyallup River valley and beyond.

Eruption Impacts

An eruption could generate pyroclastic flows, ashfall affecting regions from British Columbia to California, and devastating lahars. The USGS estimates that a major lahar could cause up to $40 billion in damage, impacting infrastructure and tens of thousands of residents living on historical lahar deposits.

Mitigation and Preparedness

The Mount Rainier Volcano Lahar Warning System, implemented by the USGS and maintained by Pierce County, aims to mitigate risks through early detection and evacuation alerts. Annual large-scale evacuation drills involving local school districts are conducted to prepare communities for potential lahar events.

Seismic Activity

Background Tremors

Seismic monitoring typically records several earthquakes monthly near Mount Rainier's summit. These are often shallow and associated with the circulation of hot fluids beneath the volcano, which likely contribute to the formation of steam vents and hot springs.

Seismic Swarms

The volcano experiences periodic seismic swarms, characterized by clusters of earthquakes over several days. While these swarms are common in volcanic regions and rarely indicate imminent eruption, significant swarms have been recorded in recent years, with the 2025 swarm being the most energetic since monitoring began.

Glaciers

Glacial Extent

Mount Rainier is the most heavily glaciated peak in the contiguous United States, featuring 29 named glaciers covering approximately 78.8 kmยฒ (30.41 sq mi) as of 2015. These glaciers hold an estimated volume of 2.9 kmยณ (0.69 cubic miles) and are crucial sources of streamflow.

Historical Fluctuations

Glacial extent has varied significantly throughout history. During the Little Ice Age (14th-19th centuries), glaciers advanced to their furthest points. Since the mid-20th century, many glaciers have experienced thinning and retreat, with some, like Stevens, Pyramid, and Van Trump glaciers, showing significant decline or even disappearing.

Glacial Outburst Floods

Glaciers on Mount Rainier can generate glacial outburst floods (jรถkulhlaups) independent of volcanic eruptions. The South Tahoma Glacier, for instance, has produced numerous floods, notably in the 1980s, 1990s, and again in August 2015, posing localized hazards.

History

Indigenous Heritage

The Mount Rainier region has been inhabited by Indigenous peoples for over 8,500 years. Archaeological evidence indicates seasonal use of subalpine meadows and landscapes for hunting and gathering, with traditions of land management through fire.

European Exploration

European exploration began with Spanish expeditions in the late 18th century, followed by British explorers like Captain James Cook and George Vancouver. The mountain was named Rainier by Vancouver in 1792. The Lewis and Clark Expedition observed the mountain in 1806.

National Park Establishment

Advocacy for preservation, including by John Muir, led to the area being designated as the Pacific Forest Reserve in 1893. In 1899, Mount Rainier National Park was established as the fifth national park in the United States, dedicated to public enjoyment and preservation.

Modern Events

In 1947, Kenneth Arnold reported sighting unidentified flying objects over Mount Rainier, a sighting that popularized the term "flying saucers." The park also features historical sites like Longmire, established around a mineral spring discovered in 1883.

Climbing

Technical Ascent

Climbing Mount Rainier is a technically demanding endeavor, requiring proficiency with specialized equipment such as crampons, ice axes, and ropes. The challenging conditions, including altitude, weather, and glacier travel, contribute to a summit success rate of approximately 50% for the estimated 10,000-11,000 annual attempts.

Primary Routes

The most frequented route is the Disappointment Cleaver Route via Camp Muir on the southeast flank. An alternative is the Emmons Glacier Route via Camp Schurman on the northeast. The Liberty Ridge Route on the north face is significantly more challenging and objectively dangerous.

Dangers & Accidents

Fatality Statistics

Mount Rainier accounts for a notable percentage of mountaineering deaths and accidents in the United States. From 1897 to 2011, 89 deaths were reported. Common causes include rock and ice fall, avalanches, falls, hypothermia, and exposure, often exacerbated by fatigue or adverse weather.

Notable Incidents

The worst mountaineering accident occurred in 1981 with the loss of 11 climbers in an avalanche on the Ingraham Glacier. More recently, in 2014, six climbers died in a fall on the Liberty Ridge route. These incidents highlight the inherent risks associated with ascending the mountain.

Recreation

Hiking and Trails

Beyond climbing, the park offers extensive opportunities for outdoor recreation. Popular activities include hiking, backcountry skiing, photography, and camping. The Wonderland Trail, a 150 km (93-mile) circumnavigation of the peak, provides access to diverse backcountry environments.

Winter Activities

During winter months, the mountain's snowfields and trails are utilized for snowshoeing and cross-country skiing, offering unique perspectives on the alpine environment.

Climate

Summit Conditions

The summit of Mount Rainier experiences an ice cap climate (Kรถppen: EF). Temperatures are consistently below freezing, with significant precipitation, primarily as snow, throughout the year. Average annual precipitation exceeds 2,200 mm (89 inches).

Climate data for Mount Rainier Summit (1991-2020 normals):

MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Max ยฐF (ยฐC)1.2 (โˆ’17.1)2.4 (โˆ’16.4)4.1 (โˆ’15.5)8.0 (โˆ’13.3)16.7 (โˆ’8.5)22.3 (โˆ’5.4)31.2 (โˆ’0.4)32.5 (0.3)24.0 (โˆ’4.4)15.4 (โˆ’9.2)4.7 (โˆ’15.2)0.2 (โˆ’17.7)13.6 (โˆ’10.2)
Min ยฐF (ยฐC)โˆ’10.0 (โˆ’23.3)โˆ’10.5 (โˆ’23.6)โˆ’9.0 (โˆ’22.8)โˆ’6.1 (โˆ’21.2)0.7 (โˆ’17.4)5.0 (โˆ’15.0)11.2 (โˆ’11.6)12.1 (โˆ’11.1)7.8 (โˆ’13.4)1.1 (โˆ’17.2)โˆ’7.4 (โˆ’21.9)โˆ’11.4 (โˆ’24.1)โˆ’1.4 (โˆ’18.5)
Precipitation (in/mm)14.09 (358)11.49 (292)11.38 (289)6.73 (171)3.62 (92)3.08 (78)1.13 (29)1.30 (33)3.01 (76)7.61 (193)12.89 (327)13.60 (345)89.93 (2284)

Camp Muir Conditions

Camp Muir, situated at 3,080 meters (10,110 feet), experiences extreme alpine conditions. Mean daily temperatures remain below freezing year-round, with recorded highs reaching up to 20.3ยฐC (68.6ยฐF) and lows down to -25.8ยฐC (-14.4ยฐF). Relative humidity is high, averaging over 60% annually.

Climate data for Camp Muir (2014-2022 normals and extremes):

MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record High ยฐF (ยฐC)47.9 (8.8)48.5 (9.2)48.0 (8.9)60.1 (15.6)53.9 (12.2)66.5 (19.2)66.8 (19.3)68.6 (20.3)64.3 (17.9)57.0 (13.9)51.3 (10.7)47.7 (8.7)68.6 (20.3)
Mean Max ยฐF (ยฐC)23.2 (โˆ’4.9)22.0 (โˆ’5.6)22.8 (โˆ’5.1)26.9 (โˆ’2.8)35.1 (1.7)40.5 (4.7)48.0 (8.9)50.0 (10.0)42.1 (5.6)34.8 (1.6)26.2 (โˆ’3.2)21.1 (โˆ’6.1)32.7 (0.4)
Mean ยฐF (ยฐC)17.7 (โˆ’7.9)15.3 (โˆ’9.3)16.4 (โˆ’8.7)20.0 (โˆ’6.7)28.4 (โˆ’2.0)34.8 (1.6)42.8 (6.0)44.4 (6.9)36.7 (2.6)29.2 (โˆ’1.6)20.5 (โˆ’6.4)15.1 (โˆ’9.4)26.8 (โˆ’2.9)
Mean Min ยฐF (ยฐC)12.6 (โˆ’10.8)9.0 (โˆ’12.8)10.8 (โˆ’11.8)14.3 (โˆ’9.8)23.1 (โˆ’4.9)29.6 (โˆ’1.3)38.5 (3.6)39.7 (4.3)31.9 (โˆ’0.1)23.8 (โˆ’4.6)14.8 (โˆ’9.6)9.5 (โˆ’12.5)21.5 (โˆ’5.8)
Record Min ยฐF (ยฐC)โˆ’11.2 (โˆ’24.0)โˆ’11.6 (โˆ’24.2)โˆ’4.3 (โˆ’20.2)โˆ’6.2 (โˆ’21.2)0.7 (โˆ’17.4)4.0 (โˆ’15.6)19.3 (โˆ’7.1)23.8 (โˆ’4.6)7.4 (โˆ’13.7)0.5 (โˆ’17.5)โˆ’3.8 (โˆ’19.9)โˆ’14.4 (โˆ’25.8)โˆ’14.4 (โˆ’25.8)
Rel. Humidity (%)72.269.769.363.563.254.442.543.054.262.371.572.561.5

Ecology

Protected Ecosystem

As a protected national park, Mount Rainier safeguards a diverse Cascade ecosystem. This environment supports numerous species, including endemic flora like the Mount Rainier lousewort and fauna such as the Cascade red fox, providing a stable habitat across its varied elevations.

Biodiversity

The mountain's ecosystem is rich in biodiversity, hosting over a thousand species of plants and fungi. It is also home to 65 mammal species, 182 bird species, 14 amphibian species, 14 fish species, and countless invertebrates, reflecting distinct life forms adapted to forest, subalpine, and alpine zones.

Flora

Wildflower Meadows

Mount Rainier is renowned for its spectacular subalpine wildflower meadows, particularly in areas like Paradise. The short growing season, dictated by late-melting snowpack, results in vibrant, concentrated blooms during the summer months.

Forest Zones

The mountain's forests range from old-growth stands, some over 1,000 years old, at lower elevations, to stunted alpine trees. Dominant species include western red-cedar, Douglas fir, western hemlock, Pacific silver fir, and various alpine fir and hemlock species at higher altitudes.

Fauna

Mammalian Life

The mountain supports a diverse mammalian population, including cougars, mountain goats, marmots, elk, and the protected Cascade red fox. Efforts are underway to reintroduce species like the Pacific fisher, which were historically extirpated.

Aquatic and Avian Life

Rivers fed by glacial melt sustain salmon and trout populations. The park's avian diversity is substantial, with many migratory species utilizing the mountain's varied habitats. Amphibians and reptiles are also present, adapted to the cooler, moist environments.

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References

References

  1.  "Mowich" is the Chinook Jargon word for "deer".
A full list of references for this article are available at the Mount Rainier Wikipedia page

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Disclaimer

Academic Integrity Notice

This content has been generated by an AI model, drawing upon publicly available data. While efforts have been made to ensure accuracy and adherence to academic standards, it is intended for educational and informational purposes only. It is not a substitute for primary source research or expert consultation.

This is not professional geological, meteorological, or safety advice. Users should consult official geological surveys, park services, and emergency management agencies for the most current and authoritative information regarding volcanic hazards, climbing conditions, and safety protocols related to Mount Rainier.

The creators of this page are not liable for any inaccuracies, omissions, or consequences arising from the use of this information.