Mount Rainier National Park

Comet Falls is a tall waterfall located on Van Trump Creek in Pierce County, Washington. The falls are thought to be the best in the Mount Rainier region.

Mount Rainier ( ray-NEER), also known as Tahoma, is a large active stratovolcano in the Cascade Range of the Pacific Northwest in the United States. The mountain is located in Mount Rainier National Park about 59 miles (95 km) south-southeast of Seattle. With an officially recognized summit elevation of 14,410 ft (4,392 m) at the Columbia Crest, it is the highest mountain in the U.S. state of Washington, the most topographically prominent mountain in the contiguous United States, and the tallest in the Cascade Volcanic Arc.

The Nisqually River is a river in west central Washington in the United States, approximately 81 miles (130 km) long. It drains part of the Cascade Range southeast of Tacoma, including the southern slope of Mount Rainier, and empties into the southern end of Puget Sound. Its outlet was designated in 1971 as the Nisqually Delta National Natural Landmark.

Mount Rainier National Park ( ray-NEER) is a national park of the United States located in southeast Pierce County and northeast Lewis County in the U.S. state of Washington. 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 km²) including all of Mount Rainier, a 14,410-foot (4,390 m) stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet (490–4,300 m). The highest point in the Cascade Range, Mount Rainier is surrounded by valleys, waterfalls, subalpine meadows, and 91,000 acres (142.2 sq mi; 368.3 km²) of old-growth forest. More than 25 glaciers descend the flanks of the volcano, which is often shrouded in clouds that dump enormous amounts of rain and snow.

Little Tahoma Peak, also called Little Tahoma, is a satellite peak of Mount Rainier in Pierce County, Washington and in Mount Rainier National Park. It is quite noticeable from Seattle over 60 miles (97 km) away.

Chinook Pass (elevation 5430 ft./1656 m.) is a pass through the Cascade Range in the state of Washington.

Dege Peak is a 7,009-foot (2,136 m) summit located in Pierce County of Washington state. It is part of the Sourdough Mountains in Mount Rainier National Park. It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington.

Mowich Lake is a lake located in the northwestern corner of Mount Rainier National Park in Washington state at an elevation of 4,929 feet (1,502 m). The name "Mowich" derives from the Chinook jargon word for deer.

Longmire, which is effectively encompassed by the Longmire Historic District, is a visitor services center in Washington State's Mount Rainier National Park, located 6.5 miles (10.5 km) east of the Nisqually Entrance. The area is in the Nisqually River valley at an elevation of 2,761 feet (842 m) between The Ramparts Ridge and the Tatoosh Range. Longmire is surrounded by old-growth Douglas fir, western red cedar and western hemlock.

The Mowich River is a river in the U.S. state of Washington. Its watershed drains a portion of the western side of Mount Rainier, part of the Cascade Range. The river has two main headwater branches, the South Mowich River and the North Mowich River. The South Mowich is significantly larger and sometimes considered the main river. The Mowich and its tributaries drain several of Mount Rainier's glaciers. The upper portion of its watershed is contained within Mount Rainier National Park. The river flows into the Puyallup River in the foothills west of Mount Rainier.

Paradise Inn is a historic hotel built in 1916 at 5,400-foot (1,600 m) on the south slope of Mount Rainier in Mount Rainier National Park in Washington, United States. The inn is named after Paradise, the area of the mountain in which it is located. The Henry M. Jackson Visitor Center and the 1920 Paradise Guide House are also at this location. The inn and guide house are where many climbers start their ascent of the mountain. The inn is listed in the National Register of Historic Places and is a major component of the Paradise Historic District. Additionally, it is part of the Mount Rainier National Historic Landmark District, which encompasses the entire park and which recognizes the park's inventory of National Park Service rustic architecture.

Skyscraper Mountain is a 7,078-foot-elevation (2,157-meter) summit in Pierce County of Washington state.

Carbon Glacier is located on the north slope of Mount Rainier in the U.S. state of Washington and is the source of the Carbon River. The snout at the glacier terminal moraine is at about 3,500 feet (1,100 m) above sea level, making it the lowest-elevation glacier in the contiguous United States. The glacier also has the greatest length (5.7 miles (9.2 km)), thickness (700 ft (210 m)) and volume (0.2 cubic miles (0.83 km³)) of any U.S. glacier outside of Alaska.

Cayuse Pass (el. 4,675 ft (1,425 m)) is a mountain pass in the Cascade Mountains in the state of Washington.

The Cowlitz Glacier is on the southeast flank of Mount Rainier in the U.S. state of Washington. The body of ice covers 1.3 square miles (3.4 km²) and has a volume of 6 billion ft³ (170 million m³). The glacier starts at an elevation of 10,700 feet (3,300 m) and flows southeast. An adjacent glacier, the Paradise Glacier, is connected to this glacier on its southwest margin. As it flows down the slopes of Mount Rainier it nearly meets up with the Ingraham Glacier and during the Little Ice Age, which ended around the year 1850, the two glaciers shared a common terminus. Meltwater from the glacier drains into the Cowlitz River.

Edmunds Glacier is located on Mount Rainier in the U.S. state of Washington. Named in 1883 for Vermont senator George F. Edmunds, the glacier lies on the western flank of the volcano below the steep, rocky Mowich Face and Sunset Face. Starting from an elevation of about 9,900 ft (3,000 m), the glacier flows northwest down to 7,000 ft (2,100 m) and ends northeast of the Jeanette Heights region of Mount Rainier. Meltwater from the Edmunds Glacier feeds the Mowich River which eventually merges with the Puyallup River.

Emmons Glacier is on the northeast flank of Mount Rainier, in Washington. At 4.3 sq mi (11 km²), it has the largest surface area of any glacier in the contiguous United States. The glacier was named after the geologist Samuel Franklin Emmons after his involvement in a survey of Mount Rainier in 1870.

Flett Glacier refers to two glaciers on the northwestern flank of Mount Rainier in the U.S. state of Washington. The glaciers lie on a subsidiary peak of Rainier, the 8,364 feet (2,549 m) Observation Rock. There are two sections of glacial ice, an eastern lobe at about 7,600 ft (2,300 m) to 7,300 ft (2,200 m) in elevation, a smaller western lobe at about 7,200 ft (2,200 m) in elevation. Meltwater from the glacier flows into the Puyallup River.

Fryingpan Glacier is on the eastern face of the 11,138-foot (3,395 m) Little Tahoma Peak, just to the east of Mount Rainier in the U.S. state of Washington. The glacier is located on top of a cliff from the Emmons Glacier to the north and a small ridge separates this glacier from the Whitman Glacier to the south, except for a small snowfield in which these two glaciers are connected. Most of the ice is located on a broad plateau at an elevation of 8,000 to 8,600 feet (2,400 to 2,600 m). The head of the Fryingpan Glacier is located to the northeast of the ridge and at the foothill of Little Tahoma Peak at around 9,100 to 9,800 feet (2,800 to 3,000 m). The glacier flows downhill eastward and the uneven topography causes the glacier surface to be crevassed The glacier ends on shallow to steep slopes at about 7,100 to 7,500 feet (2,200 to 2,300 m). Numerous snowfields and alpine meadows are located near the bottom and east of the glacier. Meltwater from the glacier drains into the White River.

The Gobbler's Knob Fire Lookout is a fire lookout tower in the extreme western region of Mount Rainier National Park at an elevation of 5,485 feet (1,672 m). One of four fire lookouts remaining in the park, the lookout is used for visitor services during summer weekends. The building is about 14 feet (4.3 m) by 14 feet (4.3 m), and was designed by the National Park Service Branch of Plans and designs under the supervision of Acting Chief Architect Edwin A. Nickel. It was built in 1933. The two-story structure features a balconied lookout on the second level, with storage on the ground level. Cables secured to deadmen keep the lookout from blowing over. The lookout was extensively damaged in a 2006 storm, along with Mount Fremont Fire Lookout. They've since been repaired.

Ingraham Glacier is on the south-eastern flank of Mount Rainier, in the U.S. state of Washington. The glacier is named for the Mount Rainier enthusiast Edward Sturgis Ingraham. From the summit ice cap, Ingraham Glacier flows east between Gibraltar Rock, (12,660 ft (3,860 m)), and Disappointment Cleaver and south of Little Tahoma Peak (11,138 ft (3,395 m)), which divides it from the much larger Emmons Glacier to the north. Descending southeast, it approaches the east flank of Cowlitz Glacier and the two glaciers nearly join at 6,700 ft (2,000 m). Meltwater from the glacier drains into the Cowlitz River.

The Cascade Volcanoes (also known as the Cascade Volcanic Arc or the Cascade Arc) are a number of volcanoes in a continental volcanic arc in western North America, extending from southwestern British Columbia through Washington and Oregon to Northern California, a distance of well over 700 miles (1,100 km). The arc formed due to subduction along the Cascadia subduction zone. Although taking its name from the Cascade Range, this term is a geologic grouping rather than a geographic one, and the Cascade Volcanoes extend north into the Coast Mountains, past the Fraser River which is the northward limit of the Cascade Range proper.

The White River Entrance to Mount Rainier National Park is a complex of buildings built between 1929 and 1931 to accommodate visitors arriving on the Yakima Park Highway, in the northeastern portion of the park. Like most of the structures in Mount Rainier, the buildings are designed in the National Park Service Rustic style, using natural stone and log materials. The historic district includes the 1933 Men's Mess Hall and Dormitory, believed to be the only surviving camp structure built by the Civilian Conservation Corps in the park.

Camp Muir, named for the naturalist John Muir, is a high-altitude refuge for climbers in Mount Rainier National Park in Washington, accessed through the Paradise Entrance. The shelters comprising the camp are situated at a 10,188 ft (3,105 m) elevation between the Muir Snowfield and the Cowlitz Glacier on Mount Rainier. Camp Muir is the most-used high camp for those attempting to climb to the mountain's summit. Camp Muir is between the Nisqually and Paradise Glaciers.

The Lake George Patrol Cabin was built in 1934 by the National Park Service in Mount Rainier National Park as a backcountry patrol station and hiker's shelter. The single-story wood-frame building measures about 26.5 feet (8.1 m) by 12 feet (3.7 m). Initially intended as a horse barn, it was converted for ranger accommodation, replacing a 1921 structure. The first cabin survived until 1969, when it was destroyed by a falling tree.

The St. Andrews Creek Bridge was built in 1930-31 as part of the West Side Road in Mount Rainier National Park. The bridge spans 26 feet (7.9 m) and is almost 34 feet (10 m) wide, carrying a two-lane road on a stone-faced concrete bridge. The West Side Road was planned to link the Nisqually and Carbon River entrances to the park, but only 13 miles (21 km) were completed in six years.

Indian Henry's Patrol Cabin is an early National Park Service patrol cabin in Mount Rainier National Park. The cabin was built in 1915–1916 at an elevation of 5,300 feet (1,600 m) in an area of the park known as "Indian Henry's Hunting Ground," which had been used in the 19th century by the Cowlitz and Nisqually tribes. "Indian Henry" was an Indian guide who accompanied James Longmire in his explorations of the area. The Indian Henry's area became a tourist destination with the 1908 establishment of the "Wigwam Camp," a tent camp which was abandoned in 1918. The area remained as a headquarters for backcountry patrols; the cabin was the first such facility in the park.

The Wonderland Trail is an approximately 93-mile (150 km) hiking trail that circumnavigates Mount Rainier in Mount Rainier National Park, Washington, United States. The trail goes over many ridges of Mount Rainier for a cumulative 22,000 feet (6,700 m) of elevation gain. The trail was built in 1915.

Cowlitz Chimneys are a group of four rhyolite towers located in Mount Rainier National Park in Pierce County of Washington state. As part of the Cascade Range, the Cowlitz Chimneys are situated southwest of Tamanos Mountain and east of Banshee Peak, all of which are visible from the Sunrise Historic District. The Sarvant Glacier is set on the north aspect of these remnants of a volcanic plug. Cowlitz is the name of several geographical features in Mount Rainier National Park, as well as the state of Washington. The name appeared as early as the Lewis and Clark journals of 1805 when it was written as "Cowliskee" and has the Chinook Jargon meaning of "capturing the medicine spirit".

Palisades Peak is a 7,040-foot (2,146 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Sourdough Mountains, a subset of the Cascade Range, and is situated 0.6 mile north of Marcus Peak. The peak's descriptive name stems from the resemblance of its columnar basalt cliffs to a palisade. Access is via Palisades Lakes Trail which starts at Sunrise Point. Access to Sunrise Point is limited due to snowpack closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. Precipitation runoff from Palisades Peak drains into the White River.

Governors Ridge is located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass and 1.09 mile east of Tamanos Mountain, which is the nearest higher peak. Precipitation runoff from Governors Ridge drains into tributaries of the White River and Cowlitz River. The toponym honors all the governors who have served the state of Washington. The highest rocky crag on the ridge is known as Governors Peak. There is also a 40-foot leaning spire known as Governors Needle, and Barrier Peak is at the southern culmination of the ridge. The normal climbing access is from the Owyhigh Lakes Trail.

The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).

Van Trump Falls is a waterfall on Van Trump Creek in Pierce County, Washington. The falls are located a short distance downstream from the mouth of Falls Creek.

The Longmire Campground Comfort Stations were built in the early and mid-1930s in Mount Rainier National Park to provide public toilet facilities to automobile tourists camping in the park at Longmire. Essentially the same in design, the facilities were designed by the National Park Service Branch of Plans and Designs. Their construction was supervised by park landscape architect Ernest A. Davidson. The timber-frame buildings followed the tenets of the prevailing National Park Service Rustic style.

The Chinook Pass Entrance Arch marks the east entrance to Mount Rainier National Park. The rectangular log entry arch is one of several placed at the entrances to the park. It was designed in 1933 by the National Park Service Branch of Plans and Designs, and was built in 1936 by the Civilian Conservation Corps. The arch consists of two stone abutments carrying horizontal logs over the road. The arch functions as a bridge, carrying a horse trail, which is now part of the Pacific Crest Trail.

The Christine Falls Bridge is a reinforced concrete arch bridge in Mount Rainier National Park, spanning Van Trump Creek at Christine Falls. The bridge was built in 1927–1928 by contractor J. D. Tobin of Portland, Oregon, who built the Narada Falls Bridge at the same time. The arch has a three-centered profile and spans 56 feet (17 m). The bridge is 30 feet (9.1 m) wide. It was faced with rubble stonework and is an example of National Park Service Rustic design.

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. It was fed by a small dam on Edith Creek, which was replaced in 1970. The chlorination house contained equipment to chlorinate the water from this source and to regulate the level of the reservoir.

The St. Andrews Patrol Cabin was built by the National Park Service in 1922 as part of a network of stations near the boundaries of Mount Rainier National Park for rangers on patrol. The one-room log structure stands along St. Andrews Creek and St. Andrews Creek Trail near the Westside Road and the western boundary of the national park. The exterior of the cabin features a porch to the front. The interior is finished with varnished logs and tongue and groove flooring. The cabin was placed on the National Register of Historic Places on March 13, 1991. It is 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.

The Paradise Ice Caves (also known as the Paradise Glacier Caves) were a system of interconnected glacier caves located within Mount Rainier's Paradise Glacier in the United States. These glacier caves were visited and documented at least as early as 1908. They have a varied natural history, as their size and even existence has changed over time, from a maximum surveyed length of 13.25 kilometers in 1978, to not existing at all during both the 1940s and 1990s due to glacial recession. In 1978 they were the longest mapped system of glacier caves in the world.

The South Puyallup River Bridge was built in 1930–31 in Mount Rainier National Park as part of the West Side Road project, planned to link the park's Nisqually and Carbon River entrances. The stone-faced reinforced concrete bridge was designed by the National Park Service and the Bureau of Public Roads. It spans 42 feet (13 m) and is almost 35 feet (11 m) wide, carrying two lanes of traffic.

The Nisqually Entrance Historic District comprises the first public entrance to Mount Rainier National Park. The district incorporates the log entrance arch typical of all Mount Rainier entrances, a log frame ranger station and checking station, a comfort station and miscellaneous service structures, all built around 1926, as well as the 1915 Superintendent's Residence and the 1908 Oscar Brown Cabin, the oldest remaining structure in the park. The buildings in the district conform to the principles of the National Park Service Rustic style that prevailed in park design of the 1920s and 1930s.

The Sourdough Mountains, also called Sourdough Ridge, is a mountain ridge on the northeast side of Mount Rainier in Mount Rainier National Park, Washington, United States. The range forms an L-shape, starting at Mount Fremont, running east to Dege Peak, turning north to Slide Mountain.

The White River Mess Hall and Dormitory is the only remaining Civilian Conservation Corps camp structure remaining in Mount Rainier National Park. The wood-framed building was built in 1933, and comprising 2,185 square feet (203.0 m²), originally containing a kitchen dining room, living room, two bathrooms, a bedroom and a bunkroom, as well as a service porch. The building no longer serves as a residence and is used for storage. It is located at the White River entrance to the park, part of a complex of service buildings.

The Tipsoo Lake Comfort Station was designed by the National Park Service Branch of Plans and Designs in the National Park Service Rustic style and built in Mount Rainier National Park by the Civilian Conservation Corps in 1934. The design was supervised by Park Service Chief Architect Thomas Chalmers Vint, and is similar to the Sunrise Comfort Station in the central portion of the park. Located near the park's northern entrance, two comfort station were planned to be part of a developed area in the vicinity of Tipsoo and Chinook Pass, which was never developed beyond the toilet facilities and an entrance arch. One of these survives and remains in use. The public toilet facility features rough stonework to window sill level, with a framed wall above and a log-framed roof with cedar shingles.

The Williwakas Glacier was a glacier located on the south flank of Mount Rainier in Washington. The glacier lies below the Paradise Glacier. Due to its relatively low elevation—6,600 feet (2,000 m)–6,900 feet (2,100 m)—the glacier is small and surrounded by small snow fields above the regional tree line. A stubby 7,163 ft (2,183 m) peak is located to the east of the glacier.

The Tahoma Vista Comfort Station was designed by the National Park Service Branch of Plans and Designs in the National Park Service Rustic style and built in Mount Rainier National Park by the Civilian Conservation Corps in 1931. The design was supervised by Park Service Chief Architect Thomas Chalmers Vint, and site selection and development were undertaken by Park Service landscape architect Ernest A. Davidson. The comfort station serves the Tahoma Vista Overlook, also designed by Davidson. The 14-foot (4.3 m) by 30-foot (9.1 m) public toilet facility features rough stonework to window sill level, with a framed wall above and a log-framed roof with cedar shingles.

The White River Bridge was built in 1929 in Mount Rainier National Park as part of the Yakima Park Road project. The new road was planned to open up access to the northeastern portion of the park. The bridge, spanning the White River, was built by contractor John D. Tobin of Portland, Oregon, who had previously built the Narada Falls Bridge and the Christine Falls Bridges, both listed on the National Register of Historic Places. Plans for the bridge were drawn by the National Park Service Branch of Plans and Designs in the National Park Service Rustic style, with construction supervision by NPS landscape architect Ernest A. Davidson. The three-centred arch spans 60 feet (18 m), with a stone-faced concrete structure.

Mother Mountain is a 6,480+ ft (1,980+ m) multi-summit, 3-mile long ridge-like mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies 7 mi (11 km) northwest of the summit of Mount Rainier. The Wonderland Trail provides one approach option to this mountain, and the summit offers views of Mount Rainier. East Fay Peak is its nearest higher neighbor, 0.42 mi (0.68 km) to the south. Precipitation runoff from Mother Mountain is drained by Cataract Creek on the south side of the mountain, and Ipsut Creek drains the north side of it, and both are tributaries of the Carbon River. The west side drains into Mowich Lake, and thence Mowich River.

The Huckleberry Creek Patrol Cabin is located in the northern portion of Mount Rainier National Park, Washington, United States. It was built around 1934 to house rangers on patrol within the park. The log cabin's design resembles the "Standard Plan for Patrol Cabins" prepared by the Western Division of the National Park Service, with the addition of a full-width front porch. Civilian Conservation Corps labor may have been used in the construction of the cabin.

Eunice Lake is a glacial lake located in Pierce County, Washington and in the northwest part of Mount Rainier National Park. The lake was named after Eunice Sargent Roth by her husband Andy (Adolph) Roth who grew up in Washogal and was active in the forest service for many years. The lake is a popular area for hiking.

Burroughs Mountain is a mountain in Pierce County, Washington, United States.

Mount Wow is a prominent 6,040+ ft (1,840+ m) mountain summit located in the southwest corner of Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies 8.6 mi (13.8 km) southwest of the summit of Mount Rainier. Its nearest higher neighbor is Iron Mountain, 3.6 mi (5.8 km) to the east-northeast. Precipitation runoff from Mount Wow is drained by Tahoma Creek on the east side of the mountain, whereas Goat Creek drains the west side of it, and both are tributaries of the Nisqually River.

Tumtum Peak is a 4,678-foot-elevation (1,426-meter) mountain summit located in the southwest corner of Mount Rainier National Park, in Pierce County of Washington state. This top-to-bottom forested peak is part of the Cascade Range and lies 8.7 mi (14.0 km) southwest of the summit of Mount Rainier. The nearest higher neighbor is Mount Wow, 2.2 mi (3.5 km) to the northwest, and Iron Mountain rises 3.56 mi (5.73 km) to the northeast. Precipitation runoff from Tumtum Peak is drained by Tahoma Creek on the west side of the mountain, whereas Kautz Creek drains the east side, and both are tributaries of the Nisqually River. The Road to Paradise traverses the southern base of the peak shortly after visitors to the park enter via the Nisqually Entrance. Topographic relief is significant as the southwest aspect rises nearly 2,500 feet (760 meters) above the road in one mile.

Barrier Peak is a small 6,521-foot (1,988-metre) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass, 0.53 mile west-northwest of Buell Peak, and 0.4 mile south-southwest of Governors Ridge, which is its nearest higher peak. Precipitation runoff from Barrier Peak drains into tributaries of the White River and Cowlitz River. The normal climbing access is from the Owyhigh Lakes Trail. The peak was so named because it served as a barrier between the Cayuse Pass region and the rest of Mount Rainier National Park.

Copper Mountain is a 6,302-foot (1,921-metre) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. Part of the Cascade Range, it is situated near the base of the Success Cleaver, overlooking Indian Henry's Hunting Ground. Its nearest neighbor is Iron Mountain 0.3 miles (0.48 km) to the south, and the nearest higher peak is Pyramid Peak, one mile (1.6 km) to the northeast. The summit provides views of Mount Rainier, Mount Adams, Mount St. Helens, and peaks of the Tatoosh Range. Precipitation runoff from Copper Mountain drains into Tahoma Creek and Fishers Horn Pipe Creek, which are both tributaries of the Nisqually River. There were great hopes in the late 1800s that mines on Mount Rainier could be a source of precious metals such as copper, silver, and gold. This landform's toponym was officially adopted in 1932 by the United States Board on Geographic Names.

Fay Peak is a double-summit mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies seven miles (11 km) northwest of the summit of Mount Rainier. The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak, 6,520+ ft (1,990+ m). Echo Rock is its nearest higher neighbor, 2.7 mi (4.3 km) to the southeast. Precipitation runoff from Fay Peak is drained by Cataract Creek on the east side of the mountain, and the west side drains into Mowich Lake and Mowich River.

Iron Mountain is a 6,286-foot (1,916-metre) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. Part of the Cascade Range, it is situated near the base of the Success Cleaver, overlooking Indian Henry's Hunting Ground. The nearest higher neighbor is Copper Mountain, 0.3 miles (0.48 km) to the north. The summit provides views of Mount Rainier, Mount Adams, Mount St. Helens, Mount Wow, and peaks of the Tatoosh Range. Precipitation runoff from Iron Mountain drains into Tahoma Creek, Devils Dream Creek, and Fishers Horn Pipe Creek, which are all tributaries of the Nisqually River. There were great hopes in the late 1800s that mines on Mount Rainier could be a source of precious metals such as copper, silver, and gold. Dark reddish rock found on Iron Mountain was thought to be iron or iron oxide. The toponym was officially adopted in 1932 by the United States Board on Geographic Names.

Marcus Peak is a 6,962-foot (2,122 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Sourdough Mountains which are a small subset of the Cascade Range, and it is situated north of Dege Peak. The peak was named in 1932 for Marcus Whitman (1802–1847), an early pioneer and physician. The Whitman Glacier on Little Tahoma also honors him. Access to Marcus Peak is limited due to snow closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. The nearest higher peak is Palisades Peak, 0.64 miles (1.03 km) to the north-northeast. Precipitation runoff from Marcus Peak drains into the White River.

McNeeley Peak is a 6,786-foot-elevation (2,068 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Sourdough Mountains, a subset of the Cascade Range. McNeeley Peak is situated north of the Sunrise Historic District, east of Mount Fremont, and northwest of Antler Peak. The peak was named in 1932 for Edwin J. McNeeley (born 1858), a prominent Tacoma businessman. Access is limited by snow closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. Precipitation runoff from McNeeley Peak drains into the White River.

Mount Fremont is a 7,214-foot-elevation (2,199 m) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. Mount Fremont is a minor peak at the southwest corner of the Sourdough Mountains which are a subset of the Cascade Range. It also the juncture for a small ridge of peaks of similar size running to the northeast. Mount Fremont is situated northwest of the Sunrise Historic District, with a popular trail leading to the Mount Fremont Fire Lookout. However, this trail does not reach the true summit which is 0.25 mi (0.40 km) north of Frozen Lake. Peak 7317, also known as Mount Fremont North, located 0.31 mi (0.50 km) west-northwest along the ridge is its nearest higher neighbor. Access is limited by snowpack closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. Precipitation runoff from Mount Fremont drains into the White River.

Shriner Peak is a 5,834-foot-elevation (1,778-meter) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated south of Cayuse Pass, southwest of Seymour Peak, and southeast of Double Peak. A four-mile trail leads from Highway 123 to the Shriner Peak Fire Lookout at the top of the mountain. Precipitation runoff from Shriner Peak drains into tributaries of the Cowlitz River.

Tamanos Mountain is a 6,790-foot (2,070 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range. Tamanos Mountain is situated west of Governors Ridge and northeast of the Cowlitz Chimneys, all of which can be seen from the Sunrise Historic District. The name tamanos derives from Chinook Jargon and has the meaning of guardian spirit. This landform's toponym was officially adopted by the U.S. Board on Geographic Names in 1932. Topographic relief is significant as the summit rises 3,100 feet (940 meters) above the White River in approximately 1.5 mile. The normal climbing access is from the Owyhigh Lakes Trail, and from the lakes scrambling up the south slope to the summit.

Tokaloo Rock is a 7,688 feet (2,343 m) mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies 4 mi (6.4 km) west of the summit of Mount Rainier, near the head of the North Puyallup River and at the foot of the Puyallup Glacier. The Wonderland Trail provides an approach to this mountain, and the summit offers views of Mount Rainier's Puyallup and Tahoma glaciers. Glacier Island is its nearest higher neighbor, 1.45 mi (2.33 km) to the southeast. Tokaloo Spire is a pillar adjacent to Tokaloo Rock and rises to an elevation of 7,471 feet (2,277 m).

Deadwood Peak is a 6,280-foot-elevation (1,910-meter) mountain summit located on the eastern border of Mount Rainier National Park. It is also situated on the shared border of Pierce County and Yakima County in Washington state. Deadwood Peak is set on the crest of the Cascade Range, immediately north of Yakima Peak and Chinook Pass, with the Pacific Crest Trail traversing its east slope. Its nearest higher peak is Naches Peak, 0.59 mi (0.95 km) to the southeast. Deadwood Peak takes its name from Deadwood Lakes and Deadwood Creek to its northwest, and their names came from the large number of downed trees in the area. From Chinook Pass, a short scramble up the south side leads to the summit with unobstructed views of Mount Rainier.

The Sunrise Comfort Station (S-310) is a comfort station in Mount Rainier National Park, Washington, USA. Built around 1930, the building was designed by Thomas Chalmers Vint of the National Park Service in association with landscape architect E.A. Davidson. The structure was part of a planned ensemble at what was then called Yakima Park, high on the northern flank of Mount Rainier. Similar structures may be found at the Ohanapecosh, Longmire and White River campgrounds in the park. The low building is framed in peeled logs on a stone foundation, set into a hillside and surrounded by native landscaping.

Panhandle Gap is a high pass in the U.S. state of Washington, on a ridge to the east of Mount Rainier, lying near the low point between Little Tahoma Peak and the Cowlitz Chimneys.

The Inter Glacier or Interglacier is a small glacier on the northeast face of Mount Rainier in Washington. As of 2021, the body of ice covers an estimated area of 0.206 square miles (0.53 km²). The glacier lies on top of a wedge called the Steamboat Prow in between the Emmons Glacier to the south and the Winthrop Glacier to the north. The glacier starts below the Steamboat Prow at about 9,400 feet (2,900 m) and flows northeast down to its moraine at 7,000 feet (2,100 m). A small subsidiary peak of Rainier, named Mount Ruth, lies adjacent to the glacier. Meltwater from the glacier is the source of the Inter Fork of the White River.

Kautz Creek is a tributary of the Nisqually River, flowing from the Kautz Glacier, with its watershed in the Mount Rainier National Park of Washington. It drains southwest from Mount Rainier for about 6 miles (9.7 km) before it joins the Nisqually River near Mount Rainier Highway. It is notable for being a severe flooding hazard due to the volume of summer glacier melt and its frequently changing course. The 400-foot (120 m) Kautz Creek Falls on the headwaters of the creek was formed by the retreat of the Kautz Glacier in the past 50 years.

The Kautz Glacier is a narrow glacier on the southern flank of Mount Rainier in Washington. Named for August Kautz, who is sometimes credited for the first ascent of Mount Rainier, covers 1.8 square miles (4.7 km²) and contains 7.8 billion ft³ (221 million m³) of ice. Upper Kautz Glacier extends south from the summit ice cap to Kautz Ice Cliff at about 11,700 feet (3,600 m). Immediately west of the main ice cliff, the glacier continues down Kautz Chute which terminates in another ice cliff just above the lower Kautz Glacier at 10,800 feet (3,300 m). Usually reached by a short descent from Camp Hazard at 11,300 feet (3,400 m) on Wapowety Cleaver, climbers following the Kautz Glacier climbing route ascend this chute to the upper glacier.

The Liberty Cap Glacier is a small glacier located near the summit of Mount Rainier, Washington. True to its name, the glacier does start at the 14,100 feet (4,300 m) Liberty Cap above the steep and rocky Sunset Amphitheater and the Mowich Face. Since the topography of Mount Rainier is very jagged and uneven, the glacier is warped and twisted during its descent northward down to its terminus at about 11,000 feet (3,400 m). From there, the glacier ice falls off the cliff and tumbles down the steep Mowich Face; eventually, this ice contributes to the large North Mowich Glacier at an elevation of 10,100 ft (3,100 m).

The Longmire Buildings in Mount Rainier National Park comprise the park's former administrative headquarters, and are among the most prominent examples of the National Park Service Rustic style in the national park system. They comprise the Longmire Community Building of 1927, the Administration Building of 1928, and the Longmire Service Station of 1929. Together, these structures were designated National Historic Landmarks on May 28, 1987. The administration and community buildings were designed by National Park Service staff under the direction of Thomas Chalmers Vint.

The Mowich Lake Patrol Cabin is one of the oldest backcountry ranger stations in Mount Rainier National Park. Built in 1922, it is located in the western portion of the park and is adjacent to the largest lake in the park. It was used by rangers on boundary patrol, and is located on the Wonderland Trail. The log cabin encloses a 15.5-foot (4.7 m) by 17.5-foot (5.3 m) area, with porch projecting 5.75 feet (1.75 m) to the front. The design was influential in the development of patrol cabin designs in the 1930s. The original foundation logs were replaced in 1974 by a crew of high school age volunteers of the Student Conservation Association.

The Mount Fremont Fire Lookout is a fire lookout in the northern region of Mount Rainier National Park at an elevation above 7,000 feet (2,100 m), the highest in the park. One of four fire lookouts remaining in the park, the lookout is used for visitor services during summer weekends. The building is about 14 by 14 feet (4.3 by 4.3 m), and was designed by the National Park Service Branch of Plans and designs under the supervision of Acting Chief Architect Edwin A. Nickel. It was built in 1933. The two-story structure features a balconied lookout on the second level, with storage on the ground level. Cables secured to deadmen keep the lookout from blowing over. The Park Service was assisted during construction by the Emergency Conservation Works Association. The lookout was extensively damaged in a 2006 storm, along with the park's Gobbler's Knob Fire Lookout. They've since been repaired.

The Ohanapecosh Glacier is small glacier located on Mount Rainier's southeastern flanks in Washington, to the east of the Whitman Crest. It covers 0.6 square miles (1.6 km²) and contains 1.3 billion ft³ (37 million m³) of ice. The glacier consists of several lobes of ice interconnected by thin snowfields. Most of the glacier lies at an elevation of 8,300 feet (2,500 m) to 7,400 feet (2,300 m), near the Whitman and the Fryingpan Glacier. Since this ice lobe ends on a cliff, it contributes ice to the lower portions of the Ohanapecosh Glacier. The lower sections of this glacier end on cliffs and a small valley at about 6,100 ft (1,900 m) in elevation. Meltwater from the glacier drains into the Ohanapecosh River and the Muddy Fork Cowlitz River, which merge downstream about four miles (6 km) outside of Mount Rainier National Park into the Cowlitz River.

The Ohanapecosh River ( oh-HAN-ə-pi-kosh) (spelled as áwxanapayk-ash in the language of the Yakima Nation and Cowlitz Tribe) is a 16-mile (26 km) river in the U.S. state of Washington.

Paradise is the name of an area at approximately 5,400 feet (1,600 m) on the south slope of Mount Rainier in Mount Rainier National Park in Washington, United States. Southeast of Seattle, the area lies on the border of Pierce and Lewis counties and includes the Paradise Valley and the Paradise Glacier, the source of the Paradise River. Paradise also offers views of Mount Rainier and the Tatoosh Range.

Paradise Glacier is a glacier on the southeast flank of Mount Rainier in Washington. It covers 0.4 square miles (1.0 km²) and contains 0.8 billion ft³ (23 million m³) with Stevens Glacier included. The glacier is bounded to the west by the Muir Snowfield, Anvil Rock and McClure Rock.

The Paradise River is a small, short but swift river in Pierce County, Washington. It is the first major tributary of the Nisqually River. Located entirely within the bounds of Mount Rainier National Park, it is notable for its waterfalls, of which there are eight.

The Puyallup Glacier is a glacier on the west flank of Mount Rainier in Washington. It covers 2.0 square miles (5.2 km²) and contains 10.2 billion ft³ (289 million m³) of ice. Sharing the same source of ice as the northern South Mowich Glacier, the Puyallup Glacier begins as a branch off the ice stream that flow out of the Sunset Amphitheater. From the split at around 8,500 feet (2,600 m), the glacier expands into a broad sheet of ice ranging from 8,400 feet (2,600 m) to 7,400 feet (2,300 m) in elevation. Leaving the large expanse of ice, the glacier flows down a small valley, it narrows significantly as it turns northwestward. From there on, the glacier is dirty and ends on steep, uneven terrain at about 6,000 ft (1,800 m). The glacier gives rise to the Puyallup River.

The Pyramid Glacier is actually a scattering of glaciers and snowfields located on the south-southwestern flank of Mount Rainier in Washington. It covers 0.2 square miles (0.5 km²) and contains 400 million ft³ (11 million m³) of ice. The glaciers lie at an elevation ranging from about 7,000 feet (2,100 m) to 9,000 ft (2,700 m). The Success Divide separates this glacier from the South Tahoma Glacier to the west. Both the Success Glacier and lower end of the Kautz Glacier border this glacier on the eastern side. Meltwater from the glacier drains into the Nisqually River.

The Russell Glacier is a medium-sized glacier on the north flank of Mount Rainier, Washington. Named for the geologist Israel Russell, it covers 1.3 square miles (3.4 km²) and contains 3.1 billion ft³ (88 million m³) of ice. Starting from its highest point at 9,400 feet (2,900 m), the Russell Glacier flows northeast towards the Carbon Glacier and contributes ice to the larger glacier before becoming distinct below 7,000 feet (2,100 m). With most of the ice located from 8,000 feet (2,400 m) to 9,000 feet (2,700 m), the glacier only descends to 6,800 feet (2,100 m), unlike the much lower extent of the Carbon Glacier. Echo Rock and 8,364 ft (2,549 m) Observation Rock, two minor sub-peaks of Rainier, lie northwest of this glacier. Meltwater from the glacier eventually reaches the Carbon River.

The Sarvant Glacier is a glacier located on the northern slopes of the Cowlitz Chimneys in the state of Washington. Named for Henry M. Sarvant, who mapped Mount Rainier in 1894, the glacier starts at an elevation of about 7,000 feet (2,100 m) and descends northward down to 6,100 ft (1,900 m). There are several patches of permanent ice and snow that lie to the east and west of the glacier. These range in elevation from about 7,000 ft (2,100 m) to 5,700 ft (1,700 m). The patches of ice and snow to the west are labeled Sarvant Glaciers.

The Shriner Peak Fire Lookout is a fire lookout tower in Mount Rainier National Park. Built in 1932 to a standard design by the National Park Service Branch of Plans and Designs, the wood-frame lookout features a ground-floor storage room and an upper-level lookout and living space with windows on all four sides. A balcony extended around the perimeter of the upper level. The Shriner Peak Lookout is one of four surviving lookout stations in the park.

The South Mowich Glacier is a glacier located on the western flank of Mount Rainier in Washington. It covers 1.4 square miles (3.6 km²) and contains 4.5 billion ft³ (127 million m³) of ice. Starting from the high-altitude cliffs above the Sunset Amphitheater at over 12,000 feet (3,700 m), the glacier flows west down Mount Rainier. The glacier is connected to the large Tahoma Glacier to the south near St. Andrews Rock at 11,000 feet (3,400 m). After leaving the Amphitheater, there is an icefall on the glacier where it plunges down below 10,000 feet (3,000 m). As the glacier descends, it gradually turns and by the time the South Mowich meets the Puyallup Glacier at 8,800 feet (2,700 m), the glacier is flowing northwest. As the glacier nears Jeanette Heights, it passes by several turns and becomes very rocky in comparison to the upper sections of the glacier. The glacier splits into two arms before their termini, with a shorter, northern arm ending at 5,500 feet (1,700 m) and the longer, larger southern arm ending near a stand of conifers at 5,100 ft (1,600 m). Meltwater from the glacier drains into the South Mowich River which eventually merges with the Puyallup River.

The South Tahoma Glacier is a glacier located on the southwest flank of Mount Rainier in State of Washington. It covers 1.1 square miles (2.8 km²) and contains 4.6 billion ft³ (130 million m³) of ice. Starting from an elevation of around 10,600 feet (3,200 m) at the base of a steep cliff, the glacier flows down southwest with the larger, adjacent Tahoma Glacier lying to the north. The smaller South Tahoma is connected to the Tahoma at an ice patch located in midway down the South Tahoma. From then on, the glacier narrows and flows down southwest and accumulates rock debris before turning and ending at an elevation of around 5,100 feet (1,600 m). The southern ice stream used to be connected to a northern ice stream coming down south from the Tahoma Glacier encompassing a jagged 7,690 feet (2,344 m) high sub-peak of Rainier called Glacier Island, but retreat has separated the glaciers at an elevation below 8,000 ft (2,400 m). Meltwater from the glacier drains into the Nisqually River.

The Success Glacier is a small glacier located on the southwestern slopes of Mount Rainier in Washington. It covers 0.3 square miles (0.8 km²) and contains 500 million cubic ft (14 million m³) of ice. The glacier is bounded to the northwest by the Success Cleaver and to the east by the Kautz Cleaver. Starting from a steep rocky slope at about 11,000 feet (3,400 m), the glacier flows southward downhill. At around 9,000 feet (2,700 m), a small snowfield joins this glacier with the Pyramid Glacier to the southwest. Soon after this point, the glacier joins the adjacent Kautz Glacier at 8,600 feet (2,600 m). The joined glaciers flow until their terminus at about 6,000 ft (1,800 m). Meltwater from the glacier drains into the Nisqually River.

The Sunrise Historic District, also known as the community of Sunrise, Washington, is located at approximately 6,400 feet (2,000 m) on a ridge overlooking the northeast side of Mount Rainier in Mount Rainier National Park. The district comprises seven individual structures designed in accordance with the principles of the National Park Service Rustic style. The area is inhabited and open to the public only during a brief period in the summer season.

The Tahoma Glacier is a long glacier mostly on the western flank of Mount Rainier in Washington. It covers 1.2 square miles (3.1 km²) and contains 4.3 billion cubic feet (120×10^⁶ m³) of ice. The glacier starts out near the summit of the volcano at over 14,200 feet (4,300 m). As the glacier flows west-southwest out of the summit area, it cascades down a steep rocky face as an icefall from 13,200 feet (4,000 m) to 11,000 feet (3,400 m), where the glacier is connected to the South Mowich Glacier to the north in the Sunset Amphitheater. As the glacier drops below 10,000 feet (3,000 m), it broadens and joins the smaller South Tahoma Glacier. After the broad expanse of ice at over 8,000 feet (2,400 m), the Tahoma Glacier narrows as it descends around the rocky 7,690-foot (2,344 m) Glacier Island, a sub-peak of Rainier once fully encircled by both the South Tahoma and Tahoma Glaciers. Leaving the bottleneck in the glacier, the glacier splits; the larger, longer northern arm continues flowing west-southwest and terminates at around 5,500 feet (1,700 m). The southern arm flows south towards the arm of the South Tahoma Glacier, but this arm terminates before it rejoins the South Tahoma at 5,700 ft (1,700 m). Meltwater from the glacier is the source of the South Puyallup River and Tahoma Creek, a tributary of the Nisqually River.

Tipsoo Lake, at an elevation of 5,298 feet (1,615 m) above sea level, is an alpine lake within the Northern Cascade Range near the summit of Chinook Pass in Pierce County, Washington.

Tolmie Peak is a 5,920+ -foot (1,800+ m) peak in the Mount Rainier area of the Cascade Range, in the U.S. state of Washington. It is located 2 miles (3.2 km) northwest of Mowich Lake, in the northwest part of Mount Rainier National Park.

The Tolmie Peak Fire Lookout is one of four fire lookout stations built in Mount Rainier National Park by the United States National Park Service (NPS) between 1932 and 1934. The two-story structure houses a lookout station on the upper level and storage at ground level. The design was prepared under the supervision of Edwin A. Nickel of the NPS Branch of Plans and Designs. The newly completed structure lost its roof to a windstorm and had to be repaired. It is secured against strong winds by cables attached to deadmen. The wood-frame structure is used as a visitor contact point on weekends.

Van Trump Creek, also called Van Trump Falls Creek or the Van Trump Fork of the Nisqually River, is a creek in Pierce County, Washington. It is a tributary of the Nisqually River, joining the river just above the mouth of the Paradise River. The creek is known for having several well known waterfalls along its course.

The Van Trump Glacier is a scattering of glaciers and snowfields located on the southern flank of Mount Rainier in Washington. Named after P. B. Van Trump, who was part of an early ascent of Mount Rainier, the glacier covers 0.2 square miles (0.5 km²) and contains 500 million ft³ (14 million m³) of ice. The glacier is located between the Wilson Glacier to the east and the Kautz Glacier to the west. The elevation of the scattering ranges from 7,000 feet (2,100 m) at the lower end to 9,800 ft (3,000 m) on the upper reaches of the glacier. Meltwater from the glacier drains into the Nisqually River.

The Whitman Glacier is a medium-sized glacier on the eastern flank of Little Tahoma Peak, a sub-peak of Mount Rainier in Washington. Named for the missionary Marcus Whitman, it covers 0.9 square miles (2.3 km²) and contains 4.4 billion ft³ (125 million m³) of ice. Starting from near the rocky spire of Little Tahoma at 10,000 feet (3,000 m), the glacier flows southeast downhill. A small snowfield connects this glacier with the adjacent Fryingpan Glacier at about 9,200 feet (2,800 m). As the Whitman Glacier flows southeast, the Whitman Crest bounds the glacier to the northeast. Upon reaching a flatter plateau at about 8,300 feet (2,500 m), the glacier does not flow far before reaching its terminus at 8,200 feet (2,500 m) to 7,800 ft (2,400 m). The small Ohanapecosh Glacier lies east of the terminus. Meltwater from the glacier drains into the Cowlitz River.

The Wilson Glacier is a medium-sized tributary glacier located on the southeast flank of Mount Rainier in Washington. Named after A.D. Wilson, who was part of an early ascent of Mount Rainier, the body of ice has an area of 0.5 square miles (1.3 km²) and has a volume of 1.9 billion feet³ (54 million m³). The glacier directly feeds ice to the adjacent, but much larger Nisqually Glacier. Starting from the head at 9,700 feet (3,000 m), the glacier flows downhill southward. One part of the glacier meets the Nisqually Glacier at 8,000 feet (2,400 m) and the other part of the glacier ends on a cliff in between the Wilson and Nisqually Glacier at 7,200 ft (2,200 m). Meltwater from the glacier feeds the Nisqually River.

The Winthrop Glacier is a large glacier on the northeastern side of Mount Rainier in Washington. Named after Theodore Winthrop, the body of ice covers 3.5 mile² (9.1 km²) and has a volume of 18.5 billion feet³ (523 million m³). Starting at over 14,300 feet (4,400 m) at the Columbia Crest, the glacier heads north and descends steeply over the uneven topography of Rainier. Another glacier, the Emmons Glacier is directly connected to this glacier up to the Steamboat Prow. After passing the Prow, the glaciers split up; the Emmons heads east-northeastward and the Winthrop continues northeast. As the terrain becomes flatter, the Winthrop glacier becomes heavily rock-covered when it terminates in a forest at about 4,900 ft (1,500 m). Meltwater from the glacier drains into the White River.

The Yakima Park Stockade Group, also known as North and South Blockhouses and Stockade at Sunrise, is a building complex consisting of four log buildings at the Sunrise Visitors Center area in the northeast part of Mount Rainier National Park. The complex is architecturally significant as a particularly fine example of rustic frontier log architecture. The first of the blockhouses and the stockade were built in 1930, while the second blockhouse followed in 1943. It was declared a National Historic Landmark in 1987. It 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.

The Paradise Historic District comprises the historic portion of Paradise developed area of Mount Rainier National Park. The subalpine district surrounds its primary structure, the Paradise Inn, a rustic-style hotel built in 1917 to accommodate visitors to the park. The Paradise Inn is a National Historic Landmark. Five other buildings are included in the district. The district was placed on the National Register of Historic Places on March 13, 1991. It is 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.

The Nisqually Glacier is one of the larger glaciers on the southwestern face of Mount Rainier in the U.S. state of Washington. The glacier is one of the most easily viewed on the mountain, and is accessible from the Paradise visitor facilities in Mount Rainier National Park. Nisqually Glacier is the source of the Nisqually River.

The North Mowich Glacier is a glacier located on the northwest flank of Mount Rainier in Washington. It covers 2.4 square miles (6.2 km²) and contains 9.5 billion ft³ (269 million m³) of ice. Starting from the foot of Rainier's steep Mowich Face at about 9,600 feet (2,900 m), the glacier first consists of two lobes of ice that flow downhill to the northwest. The southern arm of the glacier is connected to the adjacent Edmunds Glacier. As the two sections of ice join up, they form a large, relatively flat plateau of ice ranging from 7,800 feet (2,400 m) to 8,300 feet (2,500 m). This plateau is an unbroken expanse of ice except for Needle Rock, which pokes out of the glacier ice. From then on, the southern part of the glacier terminates at about 6,400 feet (2,000 m), while the northern, rocky arm flows down a glacial valley and ends at about 5,800 ft (1,800 m) in elevation. The North Mowich Glacier gives rise to the North Mowich River.

Pyramid Peak is a 6,937-foot (2,114-metre) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and overlooks Indian Henry's Hunting Ground. It is situated at the base of the Success Cleaver, south of South Tahoma Glacier, and southwest of Pyramid Glacier. The summit provides views of Mount Rainier, Mount Adams, Mount St. Helens, and peaks of the Tatoosh Range. Precipitation runoff from Pyramid Peak drains into Pyramid Creek, Tahoma Creek, and Fishers Horn Pipe Creek, which are all tributaries of the Nisqually River.