Abstract
A measurement of the six-line Mössbauer Zeeman spectrum of Fe57 in amorphous yttrium iron garnet at 4.2 K reveals a linewidth asymmetry involving the three line pairs Li and L7i, i=1, 2, 3. The major source of this asymmetry is found to be a positive correlation between isomer shift and hyperfine field with a degree of linearity of 18%. A complete linewidth analysis is given which also leads to separate estimates of the widths of the hyperfine field, isomer shift, and electric-field-gradient distributions in the glass.