A low-erosion radio frequency ion source is disclosed having a hollow body with conductive interior walls that define a cylindrical cavity, with a gas supply inlet for plasma-forming gases and a power supply inlet for injecting radio frequency energy into the cavity; an expansion chamber connected to the cavity by means of a plasma outlet hole; an ion-extraction aperture in contact with the expansion chamber; coaxial conductor disposed in the cavity, parallel to the longitudinal axis thereof, one or both ends of the coaxial conductor being in contact with a circular interior wall of the body, forming a coaxial resonant cavity; the coaxial conductor having a conductive protuberance opposite the plasma outlet hole and which extends radially into the cavity. It substantially reduces the erosion of the conductive materials.