In this paper,the authors document effort in fine-scale mapping of the 5.12 Wenchuan earthquake surface rupture on the Yingxiu-Beichuan fault near Hongkou. Surface rupture in this short stretch shows clearly large along-strike variations in both map view geometry and coseismic slips. Based on the discontinuities in slip and geometry,the rupture can be divided into four sections,from southwest to northeast.The authors also discuss the cutting relationship of slickenside striations of two different plunges and their geological and seismological implications,by pointing out that the curved striations may indicate the low initial shear stress at some localities on the Yingxiu-Beichuan fault before the Wenchuan earthquake.