During the fall of 1967, the M.I.T. Lincoln Laboratory Haystack radar was employed to study the scattering properties of the planet Venus at 3.8-cm wavelength. An increase in the transmitter power to 300kW CW and a reduction in the system noise temperature to 60°K provided a considerable improvement in the radar performance compared with that available for earlier measurements. The frequency power spectra of the echoes were determined by digital Fourier analysis of the received signals. The total power in each spectrum was computed to yield the value for the radar cross section of Venus. These average 1.75 percent of the projected area of the disk, in good agreement with a reanalysis of results obtained in 1966. The signal spectra have been averaged and employed to derive the angular scattering dependence P(