Emmons Glacier
Template:Short description Template:Use American English Template:Infobox glacier Emmons Glacier is on the northeast flank of Mount Rainier, in Washington.<ref name=topo>Template:Cite map</ref> At Template:Convert, it has the largest surface area of any glacier in the contiguous United States.<ref name=fountain>Template:Cite conference</ref> The glacier was named after the geologist Samuel Franklin Emmons after his involvement in a survey of Mount Rainier in 1870.
Starting at an elevation of over Template:Convert, the Emmons glacier flows down eastward. Near the Disappointment Cleaver at Template:Convert, the Emmons is joined by the Ingraham Glacier flowing to the south. The glaciers flow together and remain connected until they split up upon reaching the wedge of Little Tahoma Peak. As the Emmons flows northeast, the massive glacier descends until it reaches its rocky lower terminus at about Template:Convert in elevation.
In the 1930s, the glacier was found to be receding quickly. In 1963, however, a rock fall from Little Tahoma Peak covered the lower glacier with rock debris. The debris cover insulated the ice from melting. As a result of decreased melting, the glacier advanced rapidly in the early 1980s. That advance was continuing by 1992, but at a slower rate; ice beneath the rock debris was melting irregularly and forming a vast hummocky area. By 2003, the glacier was again retreating. "In the past few decades the glaciers [in the American West] have been receding, continuing a trend from the Little Ice Age."<ref name=fountain/>
Emmons Glacier is often used as a route (the Columbia Crest route) to climb to the summit of Mount Rainier. There is a Ranger Station at Camp Schurman that was established on the edge of the Steamboat Prow.
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