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By means of symmetry analysis, density functional theory calculations, and Monte Carlo simulations we show that goethite, -FeOOH, is a linear magnetoelectric below its N'{e}el temperature K. The experimentally observed magnetic field induced spin-flop phase transition results in either change of direction of electric polarization or its suppression. Calculated value of magnetoelectric coefficient is 0.24 C m T. The abundance of goethite in nature makes it arguably the most widespread magnetoelectric material.

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