The WIND and IMP 8 spacecraft detected a magnetic cloud upstream of Ea
rth's bow shock on January 10-11, 1997 while the INTERBALL-1, MAGION-4
, GEOTAIL, and LANL-084 satellites were in the vicinity of the magneto
pause and crossed it many times. Based on these multipoint observation
s we have determined the velocity of the magnetopause motion induced b
y the abrupt changes in the solar wind dynamic pressure during this ev
ent, and also the velocity of propagation through the magnetosheath of
the structures connected with the magnetic cloud. Using the determine
d velocities, we tried to find the spatial orientations and dimensions
of the observed disturbances. The estimated orientation of the interp
lanetary shock driven by the magnetic cloud is interpreted as a conseq
uence of the local deformation of the cloud surface. The timing of mea
surements made by the aforementioned satellites suggests that the stro
ng density enhancement behind the magnetic cloud is limited in spatial
extent. We attribute this enhancement to the interaction of the magne
tic cloud with the ambient solar wind plasma.