Mount Hermann

Table Mountain Glacier is in Snoqualmie National Forest in the U.S. state of Washington, to the east of Table Mountain. This small glacier is less than .50 mi (0.80 km) west of Artist Point and situated on the north slope of Table Mountain.

Iceberg Lake is a glacial lake located in Whatcom County, Washington near Mount Baker. The lake is a popular area for hiking.

Table Mountain is a Skagit Range summit located west of Mount Shuksan and northeast of Mount Baker in the North Cascades of Washington state. It is situated in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest. Table Mountain is located west of Artist Point, at the end of the Mount Baker Highway. From the Artist Point parking lot, a short 1.4 mile trail leads to the summit at the west end of the mountain. The summit offers views of Mount Shuksan, Mount Baker, Mount Hermann, and Mount Larrabee. Remnants of the Table Mountain Glacier are on the northeast slope. Precipitation runoff from the mountain drains into tributaries of the Skagit and Nooksack Rivers.

Arbuthnot Lake, Arbuthnet Lake, or Lower Chain Lake is a lake in the Mount Baker Wilderness Area, in Whatcom County, Washington, United States. It is one of the Galena Chain lakes. At one end of the lake is "Arbuthnot Falls". The lake was named in 1906.

Mazama Lakes are twin glacial lakes located in Whatcom County, Washington near Mount Baker. They are a popular area for hiking.

The Kulshan caldera is a Pleistocene volcano in the North Cascades of Washington and one of the few calderas identified in the entire Cascade Range. It is the product of the Mount Baker volcanic field, which has a history stretching back to possibly 3.722 million years ago.

Mt. Baker Ski Area is a ski resort in the northwest United States, located in Whatcom County, Washington, at the end of State Route 542. The base elevation is at 3,500 feet (1,067 m), while the peak of the resort is at 5,089 feet (1,551 m). It is about ten miles (16 km) south of the 49th parallel, the international border with Canada. Despite its name, the Mt. Baker Ski Area is actually closer to Mount Shuksan than Mount Baker. The ski area is home to the world's greatest recorded snowfall in one season, 1,140 inches (95.0 ft; 29.0 m), during the 1998–99 season. Mt. Baker also enjoys one of the highest average annual snowfall of any resort in the world, with 641 inches (53.4 ft; 16.3 m).The ski area is known for numerous challenging in-bounds routes and for the many backcountry opportunities that surround it. The backcountry is accessible from several chairlifts, and access is permitted from the resort following the Mt. Baker Ski Area backcountry policy.

Mount Ann is a 5,840-foot-elevation (1,780-meter) mountain summit located in the North Cascades in Whatcom County of Washington state. It is set within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest, and is only one mile outside the boundary of North Cascades National Park. Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker. Mount Ann can be seen south of Artist Point which is at the end of the Mount Baker Highway. Precipitation runoff from the mountain drains into Swift Creek and Shuksan Creek, which empty into Baker Lake. Topographic relief is significant as the west aspect rises 3,200 feet (980 meters) above Swift Creek in approximately one mile. The mountain is unofficially named in association with nearby Lake Ann. Due to its proximity to the Mt. Baker Ski Area, Mount Ann is a winter destination for skiing and snowshoeing.

Mount Baker Wilderness is a 119,989-acre (48,558 ha) wilderness area within the Mount Baker-Snoqualmie National Forest in the western Cascade Range of northern Washington state. Its eastern border is shared with the boundary of the Stephen Mather Wilderness and North Cascades National Park for a distance of 40 miles (65 kilometers). The wilderness extends from State Route 20 north to the Canada–US border. On the west, it is bounded by the foothills of the Puget Sound lowlands.Almost entirely within Whatcom County, the wilderness lies on the western slopes of the Cascade Mountains. The three forks of the Nooksack River and the Baker River are the major drainages of the wilderness.

White Salmon Glacier is in North Cascades National Park in the U.S. state of Washington, on the west slopes of Mount Shuksan. White Salmon Glacier is a series of small glaciers that descend to the north from a ridge feature known as Shuksan Arm. A climbers route follows the White Salmon Glacier to Fisher Chimney which provides a faster approach than others to the summit of Mount Shuksan.

Sholes Glacier is located on the northeast slopes of Mount Baker in the North Cascades of the U.S. state of Washington. The glacier lies on the north side of the ridge known as The Portals. Between 1850 and 1950, Sholes Glacier retreated 3,838 ft (1,170 m). During a cooler and wetter period from 1950 to 1979, the glacier advanced 187 ft (57 m) but between 1980 and 2006 retreated back 278 ft (85 m).Sholes Glacier is named in honor of Charles H. Sholes, who served as president of the Mazamas in the early 1900s.

Lower Curtis Glacier is in North Cascades National Park in the U.S. state of Washington. Named for photographer Asahel Curtis, the glacier is in a cirque on the western slopes of Mount Shuksan. Lower Curtis Glacier is rapidly retreating and has a negative mass balance, meaning that the rate of snow and ice that is falling in the accumulation zone is less than that which is lost each year in the ablation zone. Between 1908 and 1984, the glacier experienced a loss of thickness by 45 meters (147 ft). Between 1984 and 2002, the glacier lost another 6 meters (19 ft) in thickness. Lower Curtis Glacier also lost 28% of its surface area between the end of the little ice age (around 1850) and 1950. Between the years 1951 and 1979, the glacier actually lengthened by 245 meters (800 ft) but has retreated 184 m (600 ft) since 1985, partly due to the tongue of the glacier being on a steep precipice which may have increased the loss of ice at the termini.