  The $\Omega ^-$ magnetic moment was measured very accurately and
experimentalists remarked that it differs from the theoretical estimates, thus
posing a challenge to the latter. One such estimation uses QCDSR. We revisit
this sumrule method, using condensate parameters which were obtained from
fitting the differences ($\mu_p - \mu_n$), ($\mu_{\Sigma^+}- \mu_{\Sigma^-}$)
and ($\mu_{\Xi^0} - \mu_{\Xi^-}$) and confirm the experimental number. The
$\mu_{\Delta^{++}}$ is also found to agree with the experimental estimate.
