The structure of high-energy solar proton penetration sones in the pol
ar and subpolar regions using data from riometers, transpolar satellit
e DMSP-F6, and neutron monitors during an extremely anisotropic solar
proton event on February 16, 1984, has been studied. Particular emphas
is was placed upon interpretation of the solar proton intensity maximu
m located at the auroral and nearby latitudes. Precipitation of quasi-
trapped particles drifting along the latitudinal direction from the en
try site of the anisotropic flux at the dawnside of the magnetosphere
is discussed as a cause of this maximum.