G. Notcutt et F. Davies, DISPERSION OF GASEOUS VOLCANOGENIC FLUORIDE, ISLAND OF HAWAII, Journal of volcanology and geothermal research, 56(1-2), 1993, pp. 125-131
Fluoride was measured in samples of lichen collected in 1990 from 68 s
ites on the island of Hawaii; in addition, fluoride levels were measur
ed in 8 rainfall samples collected at the same time. The levels of flu
oride in the lichens range from 6 to 332 mug g-1, which are similar to
the levels measured on Etna. The highest levels of fluoride were dete
cted close to Kilauea, and the concentration generally decreases with
increasing distance from this volcano. This overall pattern of distrib
ution is modified by local variations in wind direction, which relate
to the topographic features of the island. Close to Kilauea, there are
more localised controls on the fluoride levels, caused by circulating
groundwaters and degassing lavas.