Abstract
The hypothesis that the Pomeranchukon consists, in part, of a pair of complex conjugate Regge poles, as suggested by Chew and Snider, is shown to allow exact exchange-degenerate fits to the high-energy total-cross-section data. A unique prediction of this hypothesis is that the ratio of real to imaginary parts for the amplitude for πpπp scattering should not rise uniformly but rather rise to plateau, remain approximately constant from pL=20 to 60 GeVc, then resume its rise.