A conductivity survey of the TAG mound was made using innovative trans
ient electric dipole-dipole instrumentation. The receiver was deployed
on the sulfide mound 30 m south of the central black smoker while the
submersible ALVIN carried the transmitter on a survey path around the
receiver at a radius of approximately 70 m. Conductivity measurements
of the seafloor between the transmitter and receiver were made at 5 m
inute intervals. The survey lasted 4 hours. Measurements made at 12 si
tes are initially interpreted in terms of an apparent conductivity of
a uniform seafloor. A more complex model in which the seafloor has two
layers is then used. Apparent conductivities range from 1.4 to 15.9 S
/m, generally higher than that of seawater. The results suggest possib
le focusing of hydrothermal convection in the northern quadrant of the
mound, adjacent zones of anhydrite accumulation and fluid convection
in the north-eastern quadrant, heterogeneity and layering in the Kreml
in zone, and unexpected spatial variability in the western quadrant. T
he data from several sites show evidence of distortion attributed to 3
-D anomalies.