Lake Assal is a crater lake in Djibouti, 155 metres below sea level and the lowest ground in Africa. The sea is ten kilometres away and gets in anyway, seeping through the rock into a basin with no outlet. Nothing leaves except water vapour, and in this heat a great deal of it does. What stays behind is brine among the saltiest on the planet, and saltier in its depths than the Dead Sea. The rest of it is crust. A sheet of white salt rings the shore, cracking and popping under your boots, and close up you can watch it building in ridges and knobs as the brine dries. Along the waterline it sorts itself into ribbons of white, grey and ochre where different minerals come out.
Wading in off the salt shelf, the water pushes back. It is dense enough to hold you at the surface, so you bob rather than swim, and it feels almost oily on the skin. Anything left in it for long comes out with a shell of white crystal on it. From the rust-red terraces above the shore the whole basin fits into one view: white pan to the horizon, navy lake below, heat haze on the mountains beyond. Afar salt cutters still work the crust by hand, prising it up in solid slabs rather than scooping it loose, and loading the slabs onto camels. A caravan can run for kilometres and takes days to reach the Ethiopian highlands, where the salt is traded for grain and coffee. All of this sits on ground that is coming apart. Three plates are pulling away from each other here, and one day the sea will stop seeping and simply flood in. In November 1978 the process showed itself: over about a week the Ardoukôba volcano fissured and the two sides of the rift jerked more than a metre apart, spilling fresh basalt. The road in crosses that lava, which is younger than most of the people driving over it.