Little Tahoma is a prominent peak in the Pacific Ranges mountain range of Washington state, USA. With an elevation of 11,138 feet, it stands as the third highest summit in the state. This glaciated peak is located east of Mount Rainier and is often considered a subsidiary peak of its larger neighbor. Little Tahoma encompasses an area of approximately 2.5 square miles and offers a challenging climb for experienced mountaineers.

During the winter season, Little Tahoma experiences significant snowpack. The snowpack range varies depending on the year and weather conditions, but it can accumulate several feet of snow, making it a popular destination for backcountry skiing and snowboarding. The melting snow runoff from Little Tahoma feeds into nearby rivers and creeks, including the Carbon River and White River, contributing to the overall water supply in the region.

The name "Little Tahoma" comes from the Native American Yakama tribe, who referred to the mountain as "Tahoma" meaning "great white mountain." The addition of "Little" differentiates it from its larger counterpart, Mount Rainier. While there is no specific lore or legends associated with Little Tahoma, its proximity to Mount Rainier and its challenging climbing routes make it a sought-after destination for mountaineering enthusiasts seeking a thrilling adventure in the Pacific Ranges.