Iron(III) chromate is the iron(III) salt of chromic acid with the chemical formula Fe<sub>2</sub>(CrO<sub>4</sub>)<sub>3</sub>.
Iron(III) chromate was discovered by Samuel Hibbert-Ware in 1817 while visiting Shetland.
It may be formed by the salt metathesis reaction of potassium chromate and iron(III) nitrate, which gives potassium nitrate as byproduct.
It also can be formed by the oxidation by air of iron and chromium oxides in a basic environment: