Daniel Barringer spent 26 years and most of his fortune drilling Meteor Crater in Arizona, convinced a giant iron meteorite lay buried under the floor. The impact had vaporized most of the meteorite, so nothing was left to find, and he died in 1929 with the shafts empty. Mineralogists honored him anyway, and in 1969, picking through a pallasite meteorite, they found a new mineral and named it barringerite, iron phosphide (Fe2P) with a share of the iron replaced by nickel.
On Earth the same compound comes out of factories. Battery makers meet it in production, because Fe2P forms inside lithium iron phosphate cathodes, where a thin conductive layer of it helps a poorly conducting material move electrons. Those cells go into electric cars and grid storage. Last year the US imported about 88,000 pounds of iron phosphide and reported producing none.