KPDS ÜDS OKUMA PARÇASI - 13

Our understanding of submarine volcanic eruptions has improved substantially in the past decade owing to the recent ability to remotely detect such events and to respond rapidly with brief surveys and sampling at the eruption site. But these data are necessarily limited to observations after the event. In contrast, the 1998 eruption of the Axial volcano on the Juan de Fuca ridge was monitored by on site sea-floor instruments. One of these instruments, which measured bottom pressure, was overrun and entrapped by the 1998 lava flow. The instrument survived and was later discovered. The data recorded by this instrument reveal the duration, character and effusion rate of an eruption on a mid-ocean ridge.