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The Edmunds Glacier is a medium-sized glacier on Mount Rainier in Washington. The body of ice covers 0.5 mile² (1.29 km²) and has a volume of 1.1 billion feet³ (31.1 million m³).[1] The glacier lies on the western flank of the volcano below the steep, rocky Mowich Face and Sunset Face. Starting from an elevation of about 9,900 feet (3,000 m), the glacier flows northwest down to 7,000 feet (2,100 m) and ends northeast of the Jeanette Heights region of Mount Rainier.[2] Meltwater from the Edmunds Glacier feeds the Mowich River which eventually merges with the Puyallup River.[1]
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