About 7,000 years ago, the Bodélé Depression was the northernmost part of Lake Megachad, an enormous body of water in north-central Africa that spanned an area larger than all the Great Lakes combined.
Today, the sandy depression and former lake bed is among the world’s most prolific sources of atmospheric dust. According to one estimate, it generates about half of the mineral dust that leaves the Sahara Desert.
On February 15, 2023, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite acquired this image of dust streaming west from the depression.
Mountain ranges northeast of the depression create a natural wind tunnel that focuses and strengthens winds as they race across fast-moving sand dunes. The dunes are comprised mainly of bits of diatomite, a light-colored sedimentary rock formed from the skeletal remains of diatoms. These common single-celled algae live in water and are encased by distinctive silica-rich cell walls.
Dust transport from the Bodélé Depression follows a semiannual cycle, with peaks in dust storms in the fall and spring. There is also a daily cycle, with the strongest winds typically blowing more dust in the morning and weaker winds blowing less dust at night.
NASA Earth Observatory image by Lauren Dauphin, using MODIS data from NASA EOSDIS LANCE and GIBS/Worldview. Story by Adam Voiland.
