Zero and longitudinal field mu SR have been used to examine the single
t ground state magnetism of the diluted magnetic semiconductor Hg1-xFe
xSe. For x greater than or equal to 0.05 mu SR experiments indicate sp
in glass behaviour which is limited to sample regions with locally enh
anced Fe2+ content. Longitudinal field spectra in the glassy state rev
eal a static local field similar to 50 mT due to induced moments of Fe
2+. These are proposed to originate from a distribution of bound magne
tic polaron energies.