A highway slope along Ailiao Creek is stroke by Typhoon Morakot in 2009. Based on multi-temporal aerial photos, digital elevation model and field investigations, several dip slope failure were confirmed in the past 70 years. The sliding masses of dip slope were formed by bedding surface and two joints. Before sliding occurr, gullies along joint direction developed. Under long-term gravitational effect, dip slope failure then triggered by daylight produced after bank erotion or highway construction. Investigation shows that dip slope failure presents various features such as deformation, buckling and sliding of rock mass according to their relative height on the slope. In response to their deformation or failure feature, the two highway passing through case slope were repaired with different engineering measures, which were proved effective after 8 years.