The South Mowich Glacier is a glacier located on the western flank of Mount Rainier in Washington. It covers 1.4 sqmi and contains 4.5 billion ft3 (127 million m3) of ice. Starting from the high-altitude cliffs above the Sunset Amphitheater at over 12000 ft, the glacier flows west down Mount Rainier. The glacier is connected to the large Tahoma Glacier to the south near St. Andrews Rock at 11000 ft. After leaving the Amphitheater, there is an icefall on the glacier where it plunges down below 10000 ft. As the glacier descends, it gradually turns and by the time the South Mowich meets the Puyallup Glacier at 8800 ft, the glacier is flowing northwest. As the glacier nears Jeanette Heights, it passes by several turns and becomes very rocky in comparison to the upper sections of the glacier. The glacier splits into two arms before their termini, with a shorter, northern arm ending at 5500 ft and the longer, larger southern arm ending near a stand of conifers at 5100 ft. Meltwater from the glacier drains into the South Mowich River which eventually merges with the Puyallup River.