We report simultaneous meteor echo observations using the Arecibo 430-MHz a
nd 46.8-MHz radars. Using identical data-taking and meteor selection criter
ia, 1868 and 367 meteors were found in the 430-MHz and 46.8-MHz beams, resp
ectively, while 145 were found in both beams during the 7 hours of observat
ion. Of the 367 VHF echoes, there were only 10 trail echoes, while the rest
were head echoes, which was quite contrary to expectation. The smaller num
ber of meteors detected by the VHF system and its wider beam width show tha
t UHF meteors are far smaller than the VHF meteors. We estimate that VHF he
ad echoes have a typical effective scattering cross section of the order of
10(-3) m(2), while the accompanying UHF echoes have an effective scatterin
g cross section of the order of 10(-6) m(2). The paucity of VHF trail echoe
s observed leads us to suggest that the ratio of head echo power to the tra
il echo power increases with decreasing meteor size. When a meteor is too s
mall, a radar can observe the head echo but not the trail echo. Of the 145
meteors observed by both radars, the powers received by the two systems wer
e not correlated. Although antenna beam pattern contributes to the lack of
correlation, it is also possible that UHF and VHF echoes may be enhanced by
different scattering mechanisms.