Algeria’s coast enjoys a Mediterranean climate with mild, wet winters. Inland, however, the terrain is mostly high desert, where mountains and transient rivers interrupt sand seas. In this dry, rugged terrain rests Tin Bider.
Geologists suspect that Tin Bider is an impact crater and estimate that it was formed in the past 70 million years, perhaps in the late Cretaceous or early Tertiary Period. Spanning 6 kilometers (4 miles), the structure sits at the southern end of a range of hills.
The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite captured this natural-color image of Tin Bider on December 3, 2010. The desert surface appears in shades of tan, camel, beige, and brown. North-facing slopes are in shadow due to the angle of sunlight from the south. That angle creates an optical illusion, making the crater look as if it sits at a lower elevation than the surrounding land. But Tin Bider actually rises above the land to the south, east, and west.
Craters may be simple or complex, depending on the impact that creates it. The elevated position and concentric rings of Tin Bider suggest that it could be a complex crater. The rings likely result from terraces composed of rock that collapsed after the impact. The underlying geology where the impact occurred, however, might also play a role.
NASA Earth Observatory image created by Jesse Allen, using EO-1 ALI data provided courtesy of the NASA EO-1 team. Caption by Michon Scott.
Acquired October 10, 2007, this false-color image shows Chiyli Crater in western Kazakhstan. Vegetation appears red, and clings primarily to riverbanks near the crater. Sunlight illuminates south-facing slopes, including the central peak of the crater.