Ww. Chadwick et al., SEABEAM DEPTH CHANGES ASSOCIATED WITH RECENT LAVA FLOWS, COAXIAL SEGMENT, JUAN-DE-FUCA RIDGE - EVIDENCE FOR MULTIPLE ERUPTIONS BETWEEN 1981-1993, Geophysical research letters, 22(2), 1995, pp. 167-170
After a swarm of earthquakes was detected on the CoAxial segment of th
e Juan de Fuca Ridge in June-July 1993, the area was resurveyed with S
eaBeam multibeam sonar to search for depth changes associated with a s
ubmarine volcanic eruption. Quantitative comparison of the 1993 SeaBea
m survey with surveys in 1981/82 and 1991 shows one area of seafloor d
epth change (up to 29 m) between 1991-93 exactly where a pristine lava
flow was discovered. In addition, two other depth anomalies (up to 37
m and 20 m) are identified between 1981-91, evidence that other recen
t eruptions have occurred along this spreading ridge segment.