We report HST/HRS observations of gas that appears to have been ejected in
the equatorial zone of eta Carinae. Some of the observed emission lines are
produced by Fe II fluorescence processes, which, for unknown reasons, are
uniquely intense near eta Carinae. Surprisingly low velocities are found, m
ost likely representing ejection events hundreds of years before the well-k
nown Great Eruption of the 1840's. Alternative interpretations are possible
with different geometrical assumptions, but they seem less straightforward
and imply a different set of novel problems. The observed velocities less
than 100 km s(-1) must be hints concerning the physical nature of eta Carin
ae; we propose one speculative scenario, combining the effects of rotation
and a modified Eddington limit. The strong fluorescent emission lines occur
only in the slowest gas, a result that we cannot yet explain. Altogether,
these data pose a number of serious theoretical questions and clues, involv
ing remarkably slow ejection speeds, formation of distinct dense condensati
ons in the ejecta, and peculiarly intense radiative excitation of certain e
mission lines.