Sluiskin Mountain

Crescent Mountain, a ridge-like peak standing at 6,715 ft (2,047 m), is located in north-central Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies 6.6 mi (10.6 km) due north of the summit of Mount Rainier. Sluiskin Mountain is its nearest higher neighbor, 0.85 mi (1.37 km) to the east. Precipitation runoff from Crescent Mountain drains west into tributaries of the Carbon River.

Old Desolate is a 7,137-foot (2,175 m) multi-summit, ridge-like mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies five miles (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 Sluiskin Mountain and Mount Rainier. Burroughs Mountain is the nearest higher neighbor, 2.37 mi (3.81 km) to the southeast. Precipitation runoff from Old Desolate drains east into the West Fork White River, or west into the Carbon River.

Mineral Mountain is a 6,503 feet (1,982 m) mountain in Mount Rainier National Park, in Pierce County of Washington state. 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 and Carbon glaciers on Mount Rainier. Old Desolate is its nearest higher neighbor, 1.16 mi (1.87 km) to the southeast.

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

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

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 lookout 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.

Mount Ruth is an 8,690-foot summit located within Mount Rainier National Park in Pierce County of Washington state. Part of the Cascade Range, Mount Ruth is situated between the Emmons Glacier and the Inter Glacier. Access is via the Glacier Basin Trail. The name of the peak honors Ruth Knapp, daughter of the prospector who built Knapp's Cabin in Glacier Basin below the peak. Precipitation runoff from Mount Ruth 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.

Willis Wall is the name given to the prominent headwall of the Carbon Glacier's eastern cirque on Mount Rainier in the state of Washington. The 3,600 feet (1,097 m) foot wall of volcanic rock on Mount Rainier's north face was named in honor of geological engineer, Bailey Willis, who helped create the first trail to the Carbon Glacier in 1881 and was also influential in securing the passage of the bill that created Mount Rainier National Park in 1899. At over a mile wide, the Carbon Glacier cirque is the largest in the Cascade Mountains. The wall itself is composed of ledges of lava, ash, consolidated breccias, and rock impregnated ice.

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. The "comfort station", otherwise known as a public toilet, 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. Another comfort station (S-005) situated between the Yakima Park Stockade Group and the Sunrise Lodge is not part of that district but contributes to the Sunrise Historic District instead. S-310 does not.

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. Starting at an elevation of over 13,800 ft (4,200 m), the Emmons glacier flows down eastward. Near the Disappointment Cleaver at 12,200 ft (3,700 m), the Emmons is joined by the Ingraham Glacier flowing to the south. The glaciers flow together and remain connected until they split up upon reaching the wedge of Little Tahoma Peak. As the Emmons flows northeast, the massive glacier descends until it reaches its rocky lower terminus at about 5,100 ft (1,600 m) in elevation. In the 1930s, the glacier was found to be receding quickly. In 1963, however, a rock fall from Little Tahoma Peak covered the lower glacier with rock debris. The debris cover insulated the ice from melting. As a result of decreased melting, the glacier advanced rapidly in the early 1980s. That advance was continuing by 1992, but at a slower rate; ice beneath the rock debris was melting irregularly and forming a vast hummocky area. By 2003, the glacier was again retreating. "In the past few decades the glaciers [in the American West] have been receding, continuing a trend from the Little Ice Age." Emmons Glacier is often used as a route (the Columbia Crest route) to climb to the summit of Mount Rainier. There is a Ranger Station at Camp Schurman that was established on the edge of the Steamboat Prow.

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.