The Tahoma Glacier is a long glacier mostly on the western flank of Mount Rainier in Washington. It covers 1.2 sqmi and contains 4.3 e9ft3 of ice. The glacier starts out near the summit of the volcano at over 14200 ft. As the glacier flows west-southwest out of the summit area, it cascades down a steep rocky face as an icefall from 13200 ft to 11000 ft, where the glacier is connected to the South Mowich Glacier to the north in the Sunset Amphitheater. As the glacier drops below 10000 ft, it broadens and joins the smaller South Tahoma Glacier. After the broad expanse of ice at over 8000 ft, the Tahoma Glacier narrows as it descends around the rocky 7690 ft 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 5500 ft. The southern arm flows south towards the arm of the South Tahoma Glacier, but this arm terminates before it rejoins the South Tahoma at 5700 ft. Meltwater from the glacier is the source of the South Puyallup River and Tahoma Creek, a tributary of the Nisqually River.