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An aeolian landform is a part of the landscape shaped by the wind. Examples of aeolian landforms include sand dunes, snow and ice structures, and areas of wind-eroded stone known as ventifacts. The term “aeolian” comes from Aeolus, the ruler of wind in Greek mythology. 

Wind can sweep sediment into formations and carry sand or ice crystals that wear down geological structures. Aeolian landforms are especially common in areas that have few obstacles to block the wind and little vegetation to hold sediment in place, such as deserts. Sometimes, aeolian landforms created by windblown deposits can become more durable if vegetation grows on top of them and secures them with systems of roots, as is common with coastal dunes. 

NASA's Earth-observing satellites collect a variety of data useful to the study of aeolian landforms, including land topography measurements and weather observations. These data help researchers understand the changing landscape of our planet and how shifts in the terrain affect ecosystems.

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Learn how to phase unwrap an interferogram — a step in analyzing topography data — in this data recipe from NASA’s Alaska Satellite Facility Distributed Active Archive Center (ASF DAAC).
Discover and Visualize Aeolian Landform Data
NASA data help us understand Earth's changing systems in more detail than ever before, and visualizations bring these data to life, making Earth science concepts accessible, beautiful, and impactful.
Data visualization is a powerful tool for analysis, trend and pattern recognition, and communication. Our resources help you find world-class data visualizations to complement and enhance your research. We also have tools and tutorials to help you translate aeolian landform data into compelling visuals.
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An aerial image of sand dunes in the Namib Desert, which abruptly stop when they hit the Kuiseb River.
Mountains of sand, some as tall as 300 meters (1000 feet), are driven by the wind across Africa’s Namib Desert. The dunes are bordered to the west by the Atlantic Ocean and in other directions by solid, rocky land. The abrupt transition from sand to land is visible in this image, acquired on November 13, 2019, by the Operational Land Imager (OLI) on Landsat 8.

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