Helium-3/helium-4 ratios in submarine basalt glasses from the Galapago
s Archipelago range up to 23 times the atmospheric ratio in the west a
nd southwest. These results indicate the presence of a relatively unde
gassed mantle plume at the Galapagos hot spot and place Galapagos alon
gside Hawaii, Iceland, and Samoa as the only localities known to have
such high helium-3/helium-4 ratios. Lower ratios across the rest of th
e Galapagos Archipelago reflect systematic variations in the degree of
dilution of the plume by entrainment of depleted material from the as
thenosphere. These spatial variations reveal the dynamics of the under
lying mantle plume and its interaction with the nearby Galapagos Sprea
ding Center.