What archaeology says
The Wabar craters are a small but genuine impact site. An iron asteroid, perhaps around fifteen metres across, broke up and struck the dunes, forming a cluster of craters (the largest about a hundred metres across) and scattering meteoritic iron together with abundant impact glass. The glass is roughly nine-tenths local sand and one-tenth meteoritic iron and nickel, and occurs as black beads, dumbbells and scoria-like fragments, wind-sorted by size across the field.
The impactor is classified as an iron meteorite, and fragments have been recovered and studied. The craters are partly buried and reshaped by moving dunes, which has complicated study and dating.
The age is genuinely uncertain. Estimates have ranged widely, from only a couple of centuries to several thousand years, with some thermoluminescence and other work favouring a very young age, possibly within the last few hundred years. There is no accepted evidence that the impact destroyed any city, and the craters are far too small to level a settlement even if one had stood there.
- A cluster of impact craters, the largest around a hundred metres wide, sits in the dunes of the Empty Quarter.
- Abundant black impact glass, about 90 percent local sand and 10 percent meteoritic iron and nickel, litters the field.
- Fragments of an iron meteorite have been recovered and classified.
- Glass beads are wind-sorted by size, decreasing with distance from the craters, as expected for an airfall of melt.
- Geophysical surveys have mapped the buried and dune-covered crater structures.
- Dating work, including thermoluminescence, points to a young age, possibly only centuries old.
