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Kego Fault is a 50 km-long northwest-trending left-lateral active fault in north Kyushu, Japan. 2005 West o# Fukuoka Prefecture Earthquake was generated from the north part of its submarine extent. We conducted single-channel seismic profiling and coring of sediments in Hakata bay in order to reveal Holocene paleoseismicity for seismic risk evaluation of the unbroken southern part of the fault, on which highly-populated Fukuoka city is developing. The active fault traces in the bay extend continuously from land, and keep same mode and sense of faulting shown on land as left-lateral strike slip with downthrown to the east. Our high-resolution seismic profile records show consistent vertical displacement down to the east along the fault traces in the Holocene sediments. Horizontally deposited layers below 2.1 m from the bay floor were successively faulted, and the layers

Holocene Paleoseismicity on Kego Fault in Hakata Bay, Northern Kyushu, Japan