The magnitude of the excess of helium, ΔC(He), generally present in waters of the Pacific Ocean and, attributed to an influx of He through the sediment‐water interface, is given by 4.3 × 1010 < ΔC(He) < 7.5 × 1010 atoms/cm³ of water. An average flux, F(He), is estimated from a simple model that assumes horizontal transport in a well mixed bottom layer, and vertical transport by advection in the water above. A value for the flux 1.9 × 106 < F(He) < 3.2 × 106 atoms/cm² sec results. A flux of this order, both relative to He³ and absolute, suggests an ionic escape mechanism for the exosphere. A comparison of the flux with the generation of He by U and Th in an oceanic crust reveals that most of the He must be derived from the mantle (∼99%), and calculations for different compositional models are in agreement with a nonchondritic earth (K/U = 1 × 104;). An elevated flux of He was found on the crest of the east Pacific rise, suggesting that the He must be transported by upward movements in the mantle material.