A current disruption (CD) event was observed by the Geotail spacecraft at (
X, Y)(GSM)=(-10.0, 1.9) R-E within 1 min from the onset of a substorm. The
event was selected as one of four near-Earth current disruption events iden
tified in a search of three years of Geotail data. Fast ion flows accompani
ed the magnetic field dipolarization, rendering this event a near-Earth bur
sty bulk flow (BBF) event. The gradient anisotropy of the 30-44 keV ions at
the onset of the flow is consistent with an Earthward motion of the heated
plasma and agrees with the direction of Aux and energy transport. The auro
ra and the associated electrojet moved from low to high latitudes during su
bstorm expansion. Our observations show that CDs and BBFs are qualitatively
similar phenomena in the near-Earth tail, both associated with poleward-mo
ving (classical) auroral substorms.