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Earth Observatory
  1. This is the hidden content, please
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  3. Fans of the Arctic
 
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Alluvial fans form along a braided river channel on Severny Island in the Russian Arctic in an image acquired on August 1, 2025, by the
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 (Operational Land Imager) on
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.
NASA Earth Observatory/Lauren Dauphin

Editor’s Note: Today’s story is the answer to the 

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.

Call it an alluvial face-off. On the southern end of Severny Island in the Russian Arctic, rivers rush down from rugged terrain flanking a broad valley. Upon reaching flatter ground, the waters slow and distribute sediment into cone-shaped features called

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. Several appear in opposing orientations alongside a braided river in this
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image.

Severny Island (Ostrov Severnyy) is a mountainous,

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landmass in the frigid high latitudes of the Northern Hemisphere. Part of the
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archipelago, the island is largely covered in glacial ice. Some glaciers, especially in the north, terminate in the sea, while others end on land, feeding meltwater into glacial streams.

Sediment-laden streams, along with the island’s topography, create favorable conditions for the formation of alluvial fans. The features typically appear at the base of steep mountain ranges, where narrow river channels open onto flatter terrain. There, rivers can slow, divide into smaller channels, and

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. Over time, the channels migrate back and forth to build up fan-shaped deposits. Dueling fans line several northwest-southeast-trending valleys in the wider view below.

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A wide view of southern Severny Island in the Russian Arctic shows ice-capped mountains interrupted by broad valleys lined with alluvial fans. The image was acquired on August 1, 2025, by the
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 (Operational Land Imager) on
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.
NASA Earth Observatory/Lauren Dauphin

Seasonal snowmelt and

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likely keep Severny’s rivers supplied with ample fan-building material.
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that higher river flows during the warmer months, driven by snowmelt, can carry more sediment out of the mountains. Glaciers also produce large volumes of eroded material as they grind downslope, some of which flushes out in meltwater.

Smaller, land-terminating mountain glaciers, like those on southern Severny Island, are particularly prone to melting as the

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. Severny’s ice is relatively understudied due to its remoteness, but satellite observations give scientists an understanding of its health. Recent analyses incorporating
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found that land-terminating glaciers across the Novaya Zemlya archipelago thinned during the
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and
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, especially at lower elevations.

NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the 

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. Story by Lindsey Doermann.

Downloads

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August 1, 2025

JPEG (19.56 MB)

References & Resources

  • Małecki, J. (2022)
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    . The Cryosphere, 16, 2067–2082.
  • Melkonian, A.K., et al. (2016)
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    . Remote Sensing of Environment, 174, 244-257.
  • NASA Earth Observatory (2009, July 30)
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    . Accessed July 13, 2026.
  • National Geographic Society (2023, October 19)
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    . Accessed July 13, 2026.
  • Science Education Resource Center, Carleton College (2026, June 9)
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    . Accessed July 13, 2026.

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