Measurements of the cosmogenic ³He (³He_c) content of various size aliquots of exposed olivines show that the fine fraction (<140 μm) has ³He_c concentrations between 14 and 100% lower than that of the coarse fractions (0.14–1 mm). Such differences attest to a grain size dependent partial release of ³He_c from the phenocrysts matrix during the preliminary in vacuo crushing. This result might have important implications since most ³He_c measurements have used for ∼20 yr a standard routine based on the fusion of bulk powdered phenocrysts, whatever their grain size. A suite of new data obtained from coarse olivine grains yielded a mean Sea Level High Latitude ³He_c production rate (SLHL P₃) of 128±5 and 136±6 at. g⁻¹ yr⁻¹, depending on the scaling factors used. This new value, which is ∼15% higher than previously published rates, is obtained from 5 ropy flow surfaces of Mt Etna (38°N) and Hawaiian (19°N) volcanoes, at elevations between sea level and 870 m and ranging in age from 1.47±0.05 to 149±23 ka according to independent ¹⁴C or K/Ar dating. ³He loss during the crushing step might account for the discrepancy between the standard reference value of 110–115 at. g⁻¹ y⁻¹ and the higher SLHL P₃ proposed here. More generally, removal of the powdered fraction before fusion is an important point to consider in further studies in order to avoid any ³He_c systematic underestimates.

An altitudinal section has also been sampled on the ropy surface of a ∼1500 yr single flow of Mauna Loa (19°N) which allowed a new empirical atmospheric attenuation length of 149±22 g cm⁻² to be documented for ³He_c in olivines between 2400 and 4000 m elevations.