Mount Ruth (Washington)

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.

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

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. Little Tahoma Peak is a volcanic remnant. It was part of a larger Mount Rainier which has eroded. The rock is quite unstable and in 1963 a large avalanche originating below it covered the lower section of Emmons Glacier with rock debris. The Fryingpan Glacier and Whitman Glacier are located just to the east of the peak. Little Tahoma Peak can most easily be accessed from Summerland, an alpine meadow area in Mount Rainier National Park. The first recorded ascent was on August 29, 1894, by JB Flett and Henry H. Garrison who climbed from Summerland using the east shoulder. If considered on its own, Little Tahoma would be the third-highest peak in Washington.

On June 21, 1981, an avalanche near Ingraham Glacier, in Mount Rainier, struck a climb party attempting to reach the summit of Mount Rainier. Out of the 29 members, 11 were killed, making it the deadliest avalanche in the history of the mountain.

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.

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.

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 Cowlitz Glacier is a glacier 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.

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.

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.