The aims of this paper are (1) briefly to describe the plasma devices
onboard the MAGION-4 satellite, launched on 3 August 1995, of the INTE
RBALL project: and (2) to discuss first observations made near the mag
netopause region. During the presented boundary crossings the MAGION-4
observed quasiperiodic pulses of magnetosheath-like plasma in a regio
n of low plasma density. This region is located just earthwards of the
magnetopause and is populated by a plasma which, except for the densi
ty, has the same parameters as in the magnetosheath. Deeper in the mag
netosphere, the encounter of a layer of hot electrons and high-energy
ions was interpreted as low-latitude boundary layer.