We report the first incoherent scatter radar observations-made at Arecibo O
bservatory-of remarkable bottom-side (< 280 km) F-region sheet-like plasma
structures with. horizontal/vertical-scales of less than or similar to1 km.
These structures are an apparent manifestation of spread-F, appear to give
rise to VHF coherent (FAI) scattering, and are clearly electrodynamic in o
rigin involving a form of the Perkins spread-F instability process in the p
resence of relatively large E-fields and horizontal plasma gradients. The n
et instability process appears to be associated with downwelling features c
haracteristic of the nighttime F-region. These structures-that may be self-
similar on scales of similar to1-100 km-indicate considerable electrodynami
c activity in the mid-latitude F-region on scales that have profound space-
weather implications especially regarding deep scintillations on earth-spac
e communications links.