Flow of turbidity currents as evidenced by failure of submarine telecommunication cables

Shu Kun Hsu, Ching Hui Tsai, Chia Yen Ku, Jean Claude Sibuet

Research output: Contribution to journalArticlepeer-review

10 Scopus citations

Abstract

Large and fast-moving turbidity currents can incise and erode continental margins and cause damage to artificial structures such as telecommunication cables on the seafloor. In this study, we show submarine landslides and turbidity currents associated with the 2006 Pingtung earthquake off SW Taiwan. Furthermore, eleven submarine cables across the Kaoping canyon and Manila trench were broken in sequence from 1500 m to 4000 m deep. We have established a full-scale calculation of the turbidity current velocities along the Kaoping canyon channel from the middle continental slope to the adjacent deep ocean. Our results show that turbidity current velocities vary downstream at steps of 20 m/s, 3.7 m/s and 5.7 m/s which demonstrates a positive relationship between turbidity current velocities and bathymetric slopes. As evidenced by the violent cable breaks happened in the 2006 Pingtung earthquakes, the destructive power of turbidity current to underwater facilities is clearly demonstrated and, in many cases, underestimated.

Original languageEnglish
Pages (from-to)167-171
Number of pages5
JournalRendiconti Online Societa Geologica Italiana
Volume7
StatePublished - 2009

Fingerprint

Dive into the research topics of 'Flow of turbidity currents as evidenced by failure of submarine telecommunication cables'. Together they form a unique fingerprint.

Cite this