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Snowy Peaks and Fall Colors in Alaska
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
Rivers of water and ice flow across the landscape north of Anchorage, Alaska, where summer is fleeting and fall arrives early. The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured this mostly cloudless, natural-color image view of the region on September 20, 2010.
Snowy peaks of the Alaska Range—Mount McKinley, among them—form an arc through the middle of the image. Though not as tall as Mount Everest when measured from sea level, McKinley has the greatest elevation between its base and summit, and it is the tallest mountain in North America.
To the south lie the Wrangell Mountains, including Mount Blackburn, and the Chugach Mountains, including Mount Witherspoon. All of the ranges are topped with networks of glaciers, some of them terminating in lakes. Glacial flour—fine particles of rock ground off nearby slopes—lends the lakes a blue-green color. West of Witherspoon and south of McKinley, a cloud bank pushes northward, nearly indistinguishable from the snow. The low-lying clouds fill valleys, roughly mimicking the shapes and colors of glaciers.
Although fall had not officially begun in the lower 48 United States, the season was well underway in Alaska by September 20, 2010, when rusts and browns predominated. Summer is short in Denali—just June and July—and autumn generally begins in August. Winter usually lasts from October through April.