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The Chihshang fault is an active reverse fault system located in the center of the Longitudinal Valley, and is a segment of the Longitudinal Valley Fault. The fault strikes north-northeast–south-southwest, situated between the Central Mountain Range and the Hai'an Range. It lies within the active major collision zone between the Philippine Sea and Eurasian plates. The Chihshang fault extends for about 35 km, from Yuli in the north to Kuanshan in the south. The Chihshang fault remains active. It is thought to be actively creeping as has continuously created cracks and fractures in walls and buildings. The Chihshang fault has a high slip rate of about 2–3 cm/year, and a 4 cm/year creep rate at the dip-slip direction approximately.
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