For hours before Waw an Namus the ground is pale sand. Then it changes. Basaltic ash lies over roughly 300 square kilometres of the Fezzan, in southern Libya — flat black grit that muffles the tyres and hints at nothing. The rim arrives without warning, and the crater drops open under you all at once, four kilometres across. A cone of loose scoria stands in the middle with an eighty-metre pit sunk into its own summit: a small volcano built inside the wreckage of a much larger one. Three salt lakes lie curled around its foot, and no two are the same colour. One is blue, one green, one a rust-red pool half hidden in a collar of reed. You walk from one to the next in minutes, through date palms, on ground that is damp underfoot in the middle of the Sahara.
The climb up it is loose scoria, half a step back for every step you take, and the top is the one place where all three line up, the black ash running out past them to the horizon. Lower down the dust smell gives way to warm brackish water, coots go up out of the reeds, and the mosquitoes find you within a minute. The name means the oasis of mosquitoes. That third of a square kilometre is a wetland in the driest desert on Earth, and waterbirds out of Europe winter on it: shoveler, teal, gadwall and little grebe. The crater has never been settled, but it was never unknown. The caravan road between Sabha and Kufra passed close by and graves lie near the lakes: in a desert this empty, permanent water is a landmark. Nobody can say when the volcano last erupted: a lava bomb from the cone dates to about 200,000 years ago, the barely eroded ash argues for a few thousand. The lakes give up water to the sun every year and are still full, and what stands in them is less than eight thousand years old, so something under this crater is putting it back.