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绵重公路103K+200～103K+400右侧山坡1979年后多次下滑。据调查此处山坡在公路通车前后都曾发生过滑塌,是稳定不久的老滑坡,位于涪江右岸的斜坡地带,滑坡后山陡立,呈一字形,约高60米,坡底近河一带流水冲刷基层外露,射洪前峰渠从岩顶载堑通过,公路建于渠上10米高处的一级台地,紧靠滑坡体前缘,几年前这处暂时处于稳定的滑坡。由于底部修渠载堑,上部开山取石,加上雨水增多和公路的加宽改善,破
Heavy road 103K + 200 ~ 103K + 400 on the right side of the hill several times after 1979 decline. According to the survey here, the slopes have occurred before and after the opening of the highway slips, is a stable old landslide, is located in the right bank of the Fujiang slope zone, the steep slope after the landslide, was shaped, about 60 meters high, near the bottom of the river Water erosion of the grassroots level exposed before the peak discharge from the rock top cutting through the highway built in the canal 10 meters high first-class platform, close to the front of the landslide body, where a few years ago in a stable landslide. As a result of the canal tributary at the bottom of the canal and the opening of the upper part of the mountain with stones, coupled with the increase of rain and the widening of roads,