Easton Glacier, Alpine glacier on Mount Baker, Washington, United States.
Easton Glacier is an expanse of ice covering Mount Baker's south slope, stretching from high altitude craters down to forested lower elevations. The frozen formation dominates the visual landscape and feeds meltwater into surrounding waterways throughout the year.
This formation developed during the last ice age as snow accumulated in the high alpine region. Since the 1800s, warming temperatures have caused significant melting and retreat of the ice mass.
The glacier bears the name of Charles F. Easton from Bellingham, who documented and preserved the historical records of Mount Baker.
Access requires hiking from trailheads at lower elevations, with routes becoming more challenging as altitude increases. Visitors need proper mountain equipment and should prepare for weather conditions that change quickly in the high alpine environment.
Bands of darker rock and debris run along the ice surface, marking where the glacier has pushed material downslope over time. These striations offer a visible record of how the ice mass continues to move despite its overall shrinkage.
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