Y. Fouquet et al., Extensive volcaniclastic deposits at the Mid-Atlantic Ridge axis: results of deep-water basaltic explosive volcanic activity?, TERRA NOVA, 10(5), 1998, pp. 280-286
A recent mapping survey followed by submersible diving investigations revea
led the existence of extensive volcaniclastic deposits on three adjoining,
progressively deeper, segments of the Mid-Atlantic Ridge, south-west of the
Azores. The maximum water depth at which subaqueous magmatic and hydro-mag
matic explosive processes can occur is controversial. This discovery provid
es fundamental constraints on the dynamics of deep subaqueous Volcanic erup
tions. Using multibeam bathymetry, sonar image interpretations, submersible
observations, volcaniclastic sample descriptions and chemical analysis, ev
idence of extensive deep water (up to -1700 m) magmatic explosive activity
of basalt at the axis of a spreading Mid-Ocean Ridge is documented for the
first time.