Certain analyses of Canadian radar studies of auroral electrojet echoes have apparently shown spectra with multiple ion cyclotron harmonic peaks. On the basis of these, it has been argued that ion cyclotron effects must be important for all echo types seen by VHF radars, not just type 3. We reject this conclusion for two reasons: (1) at the altitude of auroral backscatter (~100--120 km) the ion-neutral collision frequency is much higher than the gyro frequency-ions are essentially unmagnetized; (2) we show that the ''high resolution'' signal processing algorithm employed does not distinguish between echoes with and without harmonic structure. With a simulation, we show that the algorithm itself can impose apparent quasi-harmonic structure onto the spectrum of random noise. ¿American Geophysical Union 1991