We surveyed and sampled two active and 3 inactive mud volcanoes on the Atla
ntic continental margin of Morocco. The active mud volcanoes (named Yuma an
d Ginsburg) are each about 4 km in diameter, rise between 150-250 meters ab
ove the seafloor and are the first active methane-related mud volcanoes to
be identified in this region. The inactive volcanoes range in diameter from
1 - 3 km, with relief between 50 and 80 meters. Gravity cores from the cre
st of the active mud volcanoes yielded methane hydrates and mud breccia dep
osits. Chemosynthetic communities of Pogonophora worms and the bivalve Sole
mya were found on the surface of the active mud volcanoes. Sediment cores f
rom the inactive volcanoes contained hemipelagic sediments, rich in foramin
ifera and ahermatypic coral debris, overlying mud breccia.